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		<title>USGS Publications Warehouse</title>
		<link>https://pubs.usgs.gov</link>
		<description>New publications of the USGS.</description>
		<language>en-us</language>
		<lastBuildDate>Sun, 17 May 2026 06:40:12 +0000</lastBuildDate>
		<webmaster>https://pubs.usgs.gov/feedback</webmaster>
		<pubDate>Sun, 17 May 2026 06:40:12 +0000</pubDate>
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			<title>Distribution, abundance, breeding activities, and restoration efforts for the Southwestern Willow Flycatcher at Marine Corps Base Camp Pendleton, California—2025 Annual Report</title>
			<author>Lynn, Suellen; Howell, Scarlett; Kus, Barbara E.</author>
			<link>https://pubs.usgs.gov/publication/ofr20261016</link>
			<description>&lt;h1&gt;Executive Summary&amp;nbsp;&lt;/h1&gt;&lt;p&gt;The purpose of this report is to provide the Marine Corps with an annual summary of the distribution, abundance, and breeding activity of the endangered Southwestern Willow Flycatcher (&lt;i&gt;Empidonax traillii extimus&lt;/i&gt;; flycatcher) and to present results of management actions implemented to attract flycatchers and enhance flycatcher habitat at Marine Corps Base Camp Pendleton (MCBCP, or Base). Surveys for the flycatcher were done on Base between May 6 and July 23, 2025. All MCBCP’s historically occupied riparian habitat (core survey area) was surveyed for flycatchers in 2025. None of the non-core survey areas were surveyed in 2025.&lt;/p&gt;&lt;p&gt;No resident flycatchers were detected on Base in 2025. The one resident (female) present in 2024 did not return to the territory she occupied in 2024, and she was not detected within the historically occupied habitat surveyed in 2025.&lt;/p&gt;&lt;p&gt;Eight transient Willow Flycatchers of unknown subspecies were observed on two of the five drainages surveyed in 2025: Las Flores Creek and the Santa Margarita River. No Willow Flycatchers were detected at Fallbrook, Pilgrim, or San Mateo Creeks. Transients in 2025 occurred in mixed willow and riparian scrub habitats, dominated by multiple willow species (&lt;i&gt;Salix spp.&lt;/i&gt;). Exotic vegetation was recorded in most flycatcher locations and was dominant (cover of exotics greater than 50 percent) in more than half of all transient locations. The most common exotic plant in habitat used by flycatchers was poison hemlock (&lt;i&gt;Conium maculatum&lt;/i&gt;). All six of the flycatchers that were observed closely enough to determine banding status were unbanded.&lt;/p&gt;&lt;p&gt;Two measures were initiated in recent years to attract and retain resident breeding flycatchers on MCBCP: conspecific attraction using flycatcher song broadcasts and installation of artificial seeps to enhance flycatcher habitat. We surveyed plots with and without speakers that broadcast flycatcher vocalizations throughout the breeding season and detected two transient Willow Flycatchers within 20 meters of one speaker in 2025. We set up permanent vegetation sampling points surrounding artificial seeps and nearby sites without artificial seeps (Reference sites) to determine the effects of surface-water enhancement by seep pumps. Vegetation cover was highest near the ground and decreased with increasing height. Woody vegetation made up most of the cover at all height categories. Soil saturation in 2025 was higher at the sites near seeps than at the Reference sites and was associated with higher native herbaceous cover and lower non-native cover.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 19:40:32</pubDate>
			<category>Open-File Report</category>
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			<title>Continuous stream discharge, salinity, and associated data collected in the lower St. Johns River and its tributaries, Florida, 2023</title>
			<author>Carson, Jennifer N.; Benacquisto, Matthew T.</author>
			<link>https://pubs.usgs.gov/publication/ofr20261012</link>
			<description>&lt;p&gt;The U.S. Army Corps of Engineers, Jacksonville District, deepened the St. Johns River channel in Jacksonville, Florida, to accommodate larger, fully loaded cargo vessels. The U.S. Geological Survey (USGS), in cooperation with the U.S. Army Corps of Engineers, monitored stage, discharge, and (or) water temperature and salinity at 26 continuous data collection sites in the St. Johns River and its tributaries.&amp;nbsp;&lt;/p&gt;&lt;p&gt;This report contains information collected during the 2023 water year, from October 2022 to September 2023. Data at each site were compared for the length of the project, 8 years so far, and on a yearly basis to show the annual variability of discharge and salinity.&lt;/p&gt;&lt;p&gt;The countywide annual rainfall for the 2023 water year was below the average yearly rainfall in four of the five counties. Annual mean discharge at 9 of the 10 tributary monitoring sites was lower for the 2023 water year than for the 2022 water year, and the annual mean flow at Broward River below Biscayne Boulevard near Jacksonville, Florida (USGS site number 02246751), was the lowest recorded at that site for the 8 years of data collection. The annual mean discharge for each of the main-stem sites was higher for the 2023 water year than for the 2022 water year and was above the average for the 8 years of data collected so far.&lt;/p&gt;&lt;p&gt;Among the tributary sites, annual mean salinity was highest at Clapboard Creek above Buckhorn Bluff near Jacksonville, Fla. (USGS site number 302657081312400), the site closest to the Atlantic Ocean, and was lowest at Durbin Creek near Fruit Cove, Fla. (USGS site number 022462002), the site farthest from the ocean, for all years. Annual mean salinity data from the main-stem sites indicate that salinity decreased with distance upstream from the ocean, which was expected. Annual mean salinity for the 2023 water year was higher than or equal to that of the 2022 water year for all main-stem and tributary sites, except at St. Johns River at Dancy Point near Spuds, Fla. (USGS site number 294213081345300), which was lower. Three main-stem monitoring stations (USGS site numbers 295856081372301, 02245340, and 301057081414800) and six tributary monitoring stations (USGS site numbers 300803081354500, 022462002, 301204081434900, 02246459, 02246518, and 02246804) either had the highest annual mean salinities or tied with the highest annual mean salinities at their respective sites since data collection began.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 20:55:09</pubDate>
			<category>Open-File Report</category>
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			<title>Evaluation of stream capture related to groundwater pumping, middle Humboldt River Basin, Nevada</title>
			<author>Davis, Kyle W.; Eldridge, William; Allander, Kip; Prudic, David; Gardner, Murphy; Pavelko, Michael; Nadler, Cara</author>
			<link>https://pubs.usgs.gov/publication/pp1906</link>
			<description>&lt;p&gt;Historical, future, and potential stream capture from groundwater pumping in the middle Humboldt River Basin (MHRB), Nevada, is estimated using a calibrated numerical groundwater flow model. The model was developed to estimate (1) stream capture, which is the change in flux between the groundwater system and the Humboldt River and tributaries, and (2) change in streamflow, which is the change in streamflow estimated for the Imlay gage on the Humboldt River (U.S. Geological Survey streamgage 10333000). Historical stream capture for water years (WYs) 1961–2015 is estimated using recorded and estimated groundwater pumping during that period. Future (predictive) stream capture was based on historical stresses (WYs 1961–2015) using a scenario that simulated non-mine pumping from WY 2015 at a uniform rate for 100 years into the future. Potential stream capture throughout the middle Humboldt River Basin from groundwater pumping during varying durations of time are presented in a series of capture maps. Maps also are presented that show the potential to capture from groundwater evapotranspiration, as well as the storage changes for pumping duration of 100 years.&lt;/p&gt;&lt;p&gt;Estimates of historical stream capture from the mainstem Humboldt River during the early 1960s are less than 400 acre-feet per year (acre-ft/yr) when groundwater withdrawals and pumping rates were relatively small compared to more recent times. In the late 1980s and early 1990s, groundwater withdrawals increased and estimated historical stream capture also increased from about 4,000 acre-ft/yr in the late 1980s and early 1990s to as much as 18,800 acre-feet (acre-ft) in WY 1998. In WY 2015, estimated historical stream capture declined to about 13,000 acre-ft because of decreasing groundwater withdrawals and lower streamflow during the drought of WYs 2012–15, resulting in less stream water available for capture. Stream capture was estimated for 100 years into the future based on WY 2015 non-mine pumping rates and mine-dewatering activity through WY 2015. Stream capture is forecast to increase to about 23,000 acre-ft/yr, and streamflow in the Humboldt River could decrease by as much as 19,000 acre-ft/yr.&lt;/p&gt;&lt;p&gt;Pumping for mine-dewatering and the associated discharge of that water affects streamflow in the Humboldt River at Imlay, Nevada (U.S. Geological Survey streamgage 10333000). Historically, from WYs 1991 to 2015, streamflow was greater at Imlay gage during active mine-dewatering from mine-water discharge operations and increased by as much as 105,000 acre-ft in WY 1998. The increase was attributed mostly to the discharge of groundwater from mine-related dewatering operations directly into the mainstem Humboldt River or its tributaries, with some of this increase associated with return flows from discharge to rapid infiltration basins. Results indicate that streamflow at Imlay gage is expected to decrease by as much as 1,600 acre-ft/yr 30 years after mine-related pumping and discharge are discontinued. The streamflow reductions at the Imlay gage are expected to then decrease to around 500 acre-ft/yr, 100 years after mine-related pumping and discharge are discontinued.&lt;/p&gt;&lt;p&gt;Potential capture maps were produced for pumping durations of 10, 25, 50, and 100 years. Capture map results indicate that areas of greater potential stream capture occur adjacent to the Humboldt River and for upstream tributaries areas north of the Humboldt River.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 17:59:27</pubDate>
			<category>Professional Paper</category>
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			<title>Practical guidance for engaging end-users and experts in developing scientific tools</title>
			<author>Clements, Kaylin; English, James; Wilkins, Emily; Moore, Megan; Schuster, Rudy</author>
			<link>https://pubs.usgs.gov/publication/sir20265137</link>
			<description>&lt;p&gt;This report provides actionable guidance for scientists developing scientific tools that inform on-the-ground decision making. Scientific tools, in the context of this report, are technology or protocols that help practitioners collect and analyze their own data, and information products and web tools that practitioners could use to inform decisions. Engaging end-users and fellow experts is fundamental to the creation of useful scientific tools. Scientists can use clear and specific direction on action steps and activities to effectively engage with end-users and fellow experts during development. Our study explores lessons learned from six U.S. Geological Survey projects that designed and implemented engagement activities with end-users and experts to coproduce scientific tools for natural resource managers. U.S. Geological Survey teams engaged end-users and experts across the United States from Federal, State, and local governments; universities; Tribes; territories; and nongovernmental organizations in designing and developing scientific tools intended to support end-users in their work. An online survey with 98 participants measured satisfaction across several indicators of successful engagement, including engagement activity frequency, sufficient opportunities to provide feedback, feedback implementation, inclusion of necessary perspectives, and functionality of the tool for end-users. Semistructured interviews were held with project leads, during which the project leads reviewed a summary of the survey results. The project leads reflected on the engagement efforts used in their project, then described lessons learned from the engagement experience and participant feedback. Common themes for ensuring effective engagement identified through thematic analysis included engaging end-users during product conceptualization; establishing clear roles and expectations; considering who end-users are and how end-users may use the tool; recruiting participants through your network, boundary spanners, and leadership; understanding individual use cases; communicating how feedback was integrated into the product; and strategically using virtual meeting tools. This guide shares practical steps and exercises for planning and facilitating effective engagement based on lessons learned from project leads and case study summaries of each project.&lt;/p&gt;</description>
			<pubDate>Thu, 14 May 2026 14:21:59</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Storm surge barriers reduce seaward sediment supply to lagoonal estuaries</title>
			<author>Ralston, David; Orton, Philip; Warner, John C.; Kasaei, Shima</author>
			<link>https://pubs.usgs.gov/publication/70275725</link>
			<description>&lt;p&gt;&lt;span&gt;Numerical simulations with realistic forcing of fixed infrastructure for a proposed storm surge barrier for a lagoonal estuary, Jamaica Bay (New York, USA), are analyzed during typical forcing conditions to assess alterations to flow and sediment transport with the barrier open. Lagoonal estuaries are shallow and have modest watershed freshwater and sediment inputs, so sediment delivery is primarily from offshore by tidal transport. The storm surge barrier infrastructure across the inlet channel reduces cross-sectional area and increases tidal velocities, increasing frictional and form drag. The overall reduction in tidal amplitude is about 1%, but the quarterdiurnal M&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;component decreases by 11%. The salinity and stratification in the estuary are only slightly modified by mixing by stronger velocities near the barrier. Sediment transport in the inlet scales approximately with tidal velocity cubed and net landward transport is driven by flood-dominant tidal asymmetry. Additionally, tidal asymmetry in the jet flow through barrier openings causes a divergence in sediment transport within several kilometers. The alterations to the tidal currents reduce sediment import to the bay by 20% for fine sand; transport of sediment with slower settling velocities is less affected, with reductions of 3% for medium silt and &amp;lt;1% for fine silt. The study examined tidal exchange with an open barrier, but the overall impact also depends on barrier operations during major storm events. The impacts of barrier infrastructure on lagoonal estuaries are distinct from other estuary types due to their modest freshwater input, predominance of tidal transport, and offshore sediment supply.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 14 May 2026 13:56:24</pubDate>
			<category>Earth&apos;s Future</category>
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			<title>Salinas Valley integrated hydrologic and reservoir operations models, Monterey and San Luis Obispo Counties, California</title>
			<author>Henson, Wesley; Hanson, Randy; Boyce, Scott; Hevesi, Joseph; Earll, Marisa; Herbert, Deidre; Jachens, Elizabeth</author>
			<link>https://pubs.usgs.gov/publication/sir20265005</link>
			<description>&lt;p&gt;The area surrounding the Salinas Valley groundwater basin in Monterey and San Luis Obispo Counties of California is a highly productive agricultural area, contributes substantially to the local economy, and provides a substantial portion of vegetables and other agricultural commodities to the Nation. This region of California provides about half of the Nation’s lettuce, celery, broccoli, and spinach each year. Thus, this agricultural area provides substantial volumes of agricultural products not just for California but for the United States.&lt;/p&gt;&lt;p&gt;Changes in population and increased agricultural development, which includes a shift toward more water-intensive crops, and climate variability, have put increasing demand on both surface-water and groundwater resources in the valley. This situation has resulted in water management challenges in the Salinas Valley that generally relate to the distribution of the water supply throughout the basin. Where and when the water is present in the surface and subsurface does not coincide with where and when the water is needed. Historically, to deal with the distribution issue, water has been used conjunctively in the valley. Conjunctive use is a water management strategy that coordinates surface-water and groundwater use to maximize water availability. Groundwater is used throughout the Salinas Valley to meet water demands when surface-water supplies are insufficient. The availability of surface water is constrained by climate. Precipitation and streamflow vary seasonally and year to year. Although there are two reservoirs in the Salinas Valley to capture and store water during wet periods, the only conveyance of reservoir water to coastal agricultural areas is the Salinas River. Increasing demand for groundwater and surface-water resources throughout the Salinas Valley has resulted in undesirable effects from unsustainable water use, such as surface-water depletion, groundwater-level declines, storage depletion in the principal aquifers, and seawater intrusion. To address these escalating issues, local communities, water management agencies, and groundwater sustainability agencies are evaluating how to sustainably manage both their surface-water and groundwater resources. To meet water demands and reduce the undesirable effects of unsustainable water use, continued conjunctive management of surface water and groundwater would ideally incorporate strategies to deal with increases in demand and climate variability.&lt;/p&gt;&lt;p&gt;To evaluate the challenging water management issues in the Salinas Valley, the U.S. Geological Survey, Monterey County Water Resources Agency, and the Salinas Valley Basin Groundwater Sustainability Agency developed a comprehensive suite of models that represent the Salinas Valley hydrogeologic system called the Salinas Valley System Model. The geologic framework is known as the Salinas Valley Geologic Framework and was developed to characterize the subsurface using various topographic and geologic data sources, including information on hydrogeologic units, their surfaces and extents, geologic structures, lithology, and elevations from borehole data and cross sections, as well as details on faults and existing models. The surface-water model is called the Salinas Valley Watershed Model and simulates the Salinas River watershed. Monthly surface-water inflows into the integrated hydrologic model domain were simulated using the Salinas Valley Watershed Model. The historical model uses historical climate data, water and land use data, and reservoir releases to simulate agricultural operations, including landscape water demands, diversions, and reclaimed wastewater. The operational model adds an embedded reservoir operations framework to the simulation of the historical model that allows specified operational rules to simulate reservoir releases and changes in reservoir storage. The operational model assumes current reservoir operations and constant land use, which differs from historical conditions. Thus, the operational model is a hypothetical baseline model that can be used by local water managers to evaluate and quantify potential benefits of water supply projects. Together, the geologic framework, watershed, historical, and operational models form a tool that can be used to simulate irrigated agriculture and associated reservoir operations of the integrated hydrologic system of the Salinas Valley.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 17:52:16</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Top Elevation of Glacial Till and Thickness of the Big Sioux Aquifer Delineated From Electrical Resistivity Tomography Surveys Near Sioux Falls, South Dakota, 2022 and 2025</title>
			<author>Medler, Colton; Anderson, Todd</author>
			<link>https://pubs.usgs.gov/publication/sir20265023</link>
			<description>&lt;p&gt;The City of Sioux Falls, South Dakota, requested the U.S. Geological Survey perform electrical resistivity surveys on three parcels of land north of the city. Electrical resistivity data were collected along a total of 22 transects during March 14–18, 2022, and November 17–21, 2025. Results from electrical resistivity surveys were used to delineate the top of glacial till deposits for the purpose of characterizing the Big Sioux aquifer near the city. Delineating geologic contacts provides important information on groundwater storage, flow dynamics, well design and placement, contaminant transport, groundwater–surface-water interactions, and regional water modeling. The top elevation of glacial till and the thickness of the Big Sioux aquifer varied among the three survey areas. The interpreted top elevation of glacial till in the North survey area decreases from east to west toward a slough, with elevations ranging from 1,403 to 1,418 feet (ft). The estimated thickness of the Big Sioux aquifer in the North survey area increased from east to west, with thicknesses ranging from 23 to 38 ft. The top elevation of glacial till in the Well 72 survey area generally decreases from northwest to southeast. Top elevations of the glacial till in the Well 72 survey area ranged from 1,400 to 1,409 ft along the southern end of transect W72_2. The estimated thickness of the Big Sioux aquifer in the Well 72 survey area was greatest along a southeast to northwest trending channel, with thicknesses ranging from 28 to 40 ft. The top elevation of glacial till in the Nose survey area generally decreases west toward the Big Sioux River. Top elevations of the glacial till in the Nose survey area ranged from 1,362 to 1,395 ft. The estimated thickness of the Big Sioux aquifer in the Nose survey area ranged from 33 to 70 ft.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 17:44:04</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Watershed Continuum Monitoring Approach: Combining multiple water quality patterns along stream and river flowpaths to track sources, pathways, and processing of pollutants</title>
			<author>Kaushal, Sujay; Mon, Ashley; Grant, Stanley; Mayer, Paul; Porter, Aaron; Sekellick, Andrew; Chase, Jason Hamilton; Bhide, Shantanu; Jastram, John; Newcomer-Johnson, Tammy; Shelton, Sydney; Yaculak, Alexis; Malin, Joseph; Maas, Carly; Salanitri, Nicholas; Silberstein, Daniel; Hohman, Steven; Dann, Ashley; Slaughter, Weston; Rippy, Megan; Monofy, Ahmed; Shatkay, Ruth; Reimer, Jenna; Seppi, Madeleine; Noel, Randi; Mussa, Julianna; Kellmayer, Bennett; Sivirichi, Gwendolyn; Grese, Melissa; Boger, Walter; Chanat, Jeffrey; Duan, Shuiwang; Belt, Kenneth</author>
			<link>https://pubs.usgs.gov/publication/70275712</link>
			<description>&lt;p&gt;&lt;span&gt;There is a growing need to improve and expand water quality monitoring approaches to more accurately track the sources, fate, and transport of multiple chemicals and pollutants holistically and quantify the effects of best management practices (BMPs) at the watershed scale. An overarching question raised by scientists, environmental managers, and the general public is: how far can water quality impacts from disturbances or benefits from watershed management and restoration propagate along stream and river flowpaths? Many studies using the classic watershed approach focus on analyzing changes in water quality over time at one or a few sampling stations, whereas theories such as the River Continuum Concept focus on predicting shifts in energy sources and biological communities along rivers but have not been directly applied to water quality. We propose to merge these concepts to create a Watershed Continuum Monitoring Approach (WCMA) that combines both spatial and temporal monitoring in order to better detect and quantify trends and transitions in multiple water quality indicators along flowpaths. Specifically, an array of multiple water quality indicators are analyzed at multiple downstream points along a watershed flowpath over time. These multiple water quality indicators are analyzed together for making comparisons to infer hydrological, biological, and geochemical processes controlling sources, transport, and attenuation of pollutants (&lt;/span&gt;&lt;i&gt;e.g.&lt;/i&gt;&lt;span&gt;, analagous to stream tracer studies at the watershed scale). The WCMA leverages the natural expansion of watershed areas along a flowpath, which reflect transitions in land use, land cover, and environmental management across spatial and temporal dimensions for making direct comparisons across different stream reaches and spatial trend analysis. WCMA facilitates monitoring of multiple water quality indicators together, and identifcation of hot spots in sources and attenuation of pollutants or mixtures of pollutants. We illustrate practical applications of the WCMA to analyze water quality trends, transitions, and tradeoffs (&lt;/span&gt;&lt;i&gt;i.e.&lt;/i&gt;&lt;span&gt;, a tradeoff occurs when one pollutant is reduced but another is directly or indirectly increased downstream). We explore case studies that quantify: (1) downstream reductions in concentrations of multiple pollutants along a stream flowing to a major drinking water source due to engineered and nature-based solutions, (2) downstream reductions in multiple pollutants and water quality tradeoffs along streams experiencing stormwater BMPs and stream restoration, (3) comparisons in downstream reductions of multiple pollutants and nutrient uptake along streams draining into major drinking water sources based on types of stream restoration, (4) comparisons of downstream pollutant reductions along streams experiencing riparian forest conservation&amp;nbsp;&lt;/span&gt;&lt;i&gt;vs.&lt;/i&gt;&lt;span&gt;&amp;nbsp;stream restoration, and (5) mapping and visualizing hot spots of increasing water quality problems such as hypoxia, contaminant mobilization, and freshwater salinization that extend downstream to tidal rivers of the Chesapeake Bay. We explore future applications of WCMA for tracking decreasing trends in salinity,&amp;nbsp;&lt;/span&gt;&lt;i&gt;E. coli&lt;/i&gt;&lt;span&gt;, and other pollutants of emerging concern. WCMA can holistically inform progress towards achieving multiple water quality goals and also be used as a screening tool for selecting monitoring sites and targeting management in strategic locations. Overall, WCMA enables the simultaneous quantification and comparison of sources and transport and attenuation rates for different chemicals and pollutants across a broader range of watershed sizes and flowpath lengths, which is critical for understanding ecological, hydrological, geochemical, and biogeochemical processes along human-impacted streams and rivers.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Wed, 13 May 2026 14:33:57</pubDate>
			<category>Ecological Engineering</category>
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			<title>Effects of wildfire on soil hydraulic properties in the western Oregon Cascades</title>
			<author>Pimont, Cedric; Thaler, Evan; Ebel, Brian A.; Bladon, Kevin</author>
			<link>https://pubs.usgs.gov/publication/70275726</link>
			<description>&lt;p&gt;&lt;span&gt;Wildfires can substantially impact the hydrology of forested watersheds, increasing the risk of hydrologic hazards such as flash floods and debris flows. Soil hydraulic properties related to infiltration are a key control in determining the timing and magnitude of these hydrogeomorphic events. In our study, we collected 445 soil cores from burned (216 cores) and unburned (229 cores) reference catchments and analyzed them for soil hydraulic properties 10&amp;nbsp;months after the 2022 Cedar Creek Fire in Oregon, USA. We observed significantly greater field-saturated hydraulic conductivity (&lt;/span&gt;&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;&lt;i&gt;fs&lt;/i&gt;&lt;/sub&gt;&lt;span&gt;), sorptivity (&lt;/span&gt;&lt;i&gt;S&lt;/i&gt;&lt;span&gt;), and wetting front potential (&lt;/span&gt;&lt;i&gt;Ψ&lt;/i&gt;&lt;sub&gt;&lt;i&gt;f&lt;/i&gt;&lt;/sub&gt;&lt;span&gt;) in burned soils relative to unburned soils, with median ratios of 5.7, 4.4, and 5.0, respectively. Among low-, moderate-, and high burn severity groups, soil hydraulic properties were not statistically different. Reductions in median soil bulk density with increasing burn severity suggested an expansion of pore sizes, which may have been partially responsible for increasing&amp;nbsp;&lt;/span&gt;&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;fs&lt;/sub&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;S&lt;/i&gt;&lt;span&gt;. Additionally, in some burned soil samples, the increase in soil hydraulic properties may have been partially related to a concurrent reduction in “natural background” water repellency that is characteristic of dry, unburned soils in the Western Cascades. We observed no evidence of spatial autocorrelation in&amp;nbsp;&lt;/span&gt;&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;fs&lt;/sub&gt;&lt;span&gt;&amp;nbsp;using semivariogram analysis. Principal component analysis paired with a&amp;nbsp;&lt;/span&gt;&lt;i&gt;k-&lt;/i&gt;&lt;span&gt;means cluster analysis suggested that soil physical properties explained variations in soil hydraulic properties better than landscape attributes. Although there is a lack of regional results for comparison, our results trend in the opposite direction from drier, lower net primary productivity regions that are typically studied for post-wildfire soil hydraulic properties.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 14 May 2026 13:32:52</pubDate>
			<category>JGR Biogeosciences</category>
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			<title>Hydrogeologic framework and conceptual groundwater-flow model of the panhandle and northwest parts of the High Plains (Ogallala) aquifer in Oklahoma, 1998–2022</title>
			<author>Morris, Amy S.; Baciocco, Colin A.; Dale, Isaac A.; Codner, Chloe; Kirby, Ethan A.; Graves, Grant M.; Wagner, Derrick; Eric G. Fiorentino, ; LePera, Alan; Sanford, Jon; Joy, Lara</author>
			<link>https://pubs.usgs.gov/publication/sir20265009</link>
			<description>&lt;p&gt;This study was conducted by the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, to update the hydrogeologic framework and conceptual flow model for the panhandle and northwest parts of the High Plains (Ogallala) aquifer in Oklahoma, which together compose the Ogallala aquifer focus area. The study included the construction of a potentiometric surface, and available geologic and hydrologic data were used to evaluate saturated thickness of the aquifer. The water budget for the updated conceptual groundwater-​flow model was based on estimated inflows and outflows for the 1998–2022 study period.&lt;/p&gt;&lt;p&gt;Saturated thickness of the Ogallala aquifer averaged 127 and 116 feet for the panhandle and northwest parts, respectively. Groundwater withdrawals from the Ogallala aquifer for 1998–2022 averaged 422,054 and 39,645 acre-feet per year (acre-ft/yr) for the panhandle and northwest parts, respectively. Recharge, the primary inflow, was estimated at 0.63 inch per year for the 1998–2022 study period, with the panhandle part of the Ogallala aquifer receiving 175,068 acre-ft/yr and the northwest part of the Ogallala aquifer receiving 49,376 acre-ft/yr. Additional inflows included irrigation return flows, estimated at 8,111 and 642 acre-ft/yr for the panhandle and northwest parts, respectively, of the Ogallala aquifer. Net lateral groundwater flows, considered to be aquifer outflows, were estimated to account for 31,908 acre-ft/yr for the Ogallala aquifer focus area. Streambed seepage, which was an outflow of 5,535 acre-ft/yr, was only present in the northwest part of the Ogallala aquifer. Vertical leakage and saturated-zone evapotranspiration were considered negligible outflows. These findings provide a revised conceptual groundwater-flow model water budget for the Ogallala aquifer focus area in Oklahoma.&lt;br&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 17:07:27</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Hazard potential of compound flooding from rainfall, storm surge, and groundwater in coastal New York and Connecticut</title>
			<author>Glas, Robin; Herdman, Liv; Cook, Salme; Howlader, Archi; Masterson, Kristina Kirkyla</author>
			<link>https://pubs.usgs.gov/publication/70272659</link>
			<description>&lt;p&gt;&lt;span&gt;Compound flood events, the co-occurrence of multiple flood drivers, can result in flood hazard potential exceeding that of any single driver alone. To evaluate compound flooding in a semi-urbanized coastal area, historical records dating back to 1970 are used to study the co-occurrences of high precipitation, storm surge, and shallow groundwater conditions along the coastlines of New York and Connecticut. Joint return periods for coincident precipitation-surge events were computed using statistical dependence models and compared to the assumption of independence as a ratio, referred to here as a return period adjustment. Results indicate distinct seasonality where compound events in the area disproportionately occur in the cold season between October and April. Return period adjustments range from a factor of 1 to almost 9, demonstrating the range in precipitation-storm surge dependence across the study area. Across all 24 station triad locations, groundwater levels were elevated during times of precipitation- surge co-occurrence, reflecting the tendency for coastal storms and shallow groundwater conditions to co-occur seasonally. The result is a pseudo-trivariate compound flood hazard score and corresponding hazard map that integrates dependence between daily precipitation-surge events and overall monthly groundwater levels (as a precondition) into a relative compound hazard score. The location with the highest compound flood hazard score is on the south shore of Long Island, as well as locations across coastal Connecticut where groundwater levels compound the co-occurrence of heavy precipitation and storm surge.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 15:47:26</pubDate>
			<category>Natural Hazards and Earth System Sciences</category>
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			<title>Variability and consistency in wildfire susceptibility: Insights from a national compilation</title>
			<author>Russell, Aaron Daniel; Bair, Lucas; Meldrum, James; Hawbaker, Todd</author>
			<link>https://pubs.usgs.gov/publication/70275735</link>
			<description>&lt;div class=&quot;title&quot;&gt;Background&lt;/div&gt;&lt;p&gt;Wildfire risk in the United States is rising and remains a land management priority. The quantitative wildfire risk assessment (QWRA) framework integrates fuels, topography, weather and values at risk to estimate the potential change in value from wildfire. Within this, response functions (RFs) represent how values respond to fire intensity. These are often based on expert judgment, but variation across assessments is unclear.&lt;/p&gt;&lt;div class=&quot;title&quot;&gt;Aims&lt;/div&gt;&lt;p&gt;This study uses data from the US Geological Survey (USGS) Wildfire Hazard and Risk Assessment Clearinghouse to characterize consistency and variation across categories and contexts.&lt;/p&gt;&lt;div class=&quot;title&quot;&gt;Methods&lt;/div&gt;&lt;p&gt;We applied descriptive statistics to summarize RFs, using tables, box-and-whisker plots and heat maps stratified by highly valued resource or asset (HVRA) category and spatial scale.&lt;/p&gt;&lt;div class=&quot;title&quot;&gt;Key results&lt;/div&gt;&lt;p&gt;RFs and value definitions vary, especially for ecosystem-related resources. Some functions, such as for buildings in the wildland–urban interface (WUI), translate well across contexts, while others require more input.&lt;/p&gt;&lt;div class=&quot;title&quot;&gt;Conclusions&lt;/div&gt;&lt;p&gt;Some functions are broadly transferable, while others need customization. This analysis provides references and starting points for improvement to RFs in QWRAs.&lt;/p&gt;&lt;div class=&quot;title&quot;&gt;Interpretations&lt;/div&gt;&lt;p&gt;Expanding the clearinghouse and dataset and building more transparency in expert elicitation can build trust among communities, agencies and end-users, and can support efficient use of limited resources to mitigate wildfire risk.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 13:16:54</pubDate>
			<category>International Journal of Wildland Fire</category>
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			<title>Patterns of floodplain forest mortality and recruitment along the Upper Mississippi and Illinois Rivers: Associations with forest fragmentation and flood inundation</title>
			<author>De Jager, Nathan; Rohweder, Jason; Van Appledorn, Molly; Weiss, Shelby; Trumper, Matthew; Guyon, Lyle</author>
			<link>https://pubs.usgs.gov/publication/70275703</link>
			<description>&lt;h3 class=&quot;c-article__sub-heading&quot; data-test=&quot;abstract-sub-heading&quot;&gt;Context&lt;/h3&gt;&lt;p&gt;Different rates of floodplain forest recruitment and mortality can reveal important changes in ecosystem processes that drive forest dynamics, resulting in net changes in forest cover, thereby influencing a wide range of river habitat and morphological characteristics.&lt;/p&gt;&lt;h3 class=&quot;c-article__sub-heading&quot; data-test=&quot;abstract-sub-heading&quot;&gt;Objectives&lt;/h3&gt;&lt;p&gt;We evaluated characteristics of forest change areas in the Upper Mississippi River System.&lt;/p&gt;&lt;h3 class=&quot;c-article__sub-heading&quot; data-test=&quot;abstract-sub-heading&quot;&gt;Methods&lt;/h3&gt;&lt;p&gt;An overlay technique was used to map patches of forest loss, gain, and persistence between 2010 and 2020 in relation to a series of explanatory variables.&lt;/p&gt;&lt;h3 class=&quot;c-article__sub-heading&quot; data-test=&quot;abstract-sub-heading&quot;&gt;Results&lt;/h3&gt;&lt;p&gt;We quantified a net decline in forest cover ranging from 3.2 to 16.8% in the uppermost five study reaches, and a net increase in forest cover ranging from 0.5 to 4.6% in the southernmost three reaches. Patches of forest loss and persistence were similarly tall (&amp;gt; 15&amp;nbsp;m), dense (&amp;gt; 90% cover), silver maple (&lt;i&gt;Acer saccharinum&lt;/i&gt;) dominated forests, whereas forest gain patches were short (&amp;lt; 15&amp;nbsp;m), less dense (&amp;lt; 66% cover) and more likely to be dominated by willow (&lt;i&gt;Salix)&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;species. Both forest loss and gain patches were smaller than forest persistence patches and were typically found in areas with low neighborhood forest density (&amp;lt; 50% forested 10&amp;nbsp;ha neighborhood). Areas that experienced more than three flood events per growing season, more than 100 consecutive days of inundation during a single flood event, and more than 60 mean total days of inundation per growing season from 2011 to 2020 showed a net loss of forest cover in all study reaches. In contrast, net increases in forest cover were restricted to areas that experienced less than a single flood event per growing season, less than 40 consecutive days of inundation during a single flood event and less than 30 mean total days of inundation per growing season from 2011 to 2020.&lt;/p&gt;&lt;h3 class=&quot;c-article__sub-heading&quot; data-test=&quot;abstract-sub-heading&quot;&gt;Conclusions&lt;/h3&gt;&lt;p&gt;Forest mortality along these river reaches is associated with forest fragmentation and an increasingly wetter hydrological regime.&lt;/p&gt;</description>
			<pubDate>Wed, 13 May 2026 14:23:56</pubDate>
			<category>Landscape Ecology</category>
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			<title>Temporal and spatial changes in seismic attenuation associated with inferred fluid migration in the 2016 central Apennines earthquake sequence</title>
			<author>Malagnini, Luca; Lucente, Francesco; Munafo, Irene; Dreger, Douglas; Parsons, Thomas; Burgmann, Roland</author>
			<link>https://pubs.usgs.gov/publication/70275733</link>
			<description>&lt;p&gt;&lt;span&gt;Prior work suggests that high‐frequency seismic attenuation acts as a highly sensitive proxy for crustal permeability and fluid mobility in fractured media. We test the hypothesis that the fault system responsible for the 2016–2017 Amatrice–Visso–Norcia–Capitignano sequence acted as an impermeable seal, compartmentalizing pressurized fluids until dynamic rupture triggered widespread fluid diffusion. By tracking across the sequence the spatiotemporal evolution of the&amp;nbsp;&lt;/span&gt;&lt;i&gt;S&lt;/i&gt;&lt;span&gt;‐wave anelastic attenuation parameter, we identify large, positive low‐frequency attenuation anomalies emerging within the hanging wall following the Amatrice mainshock and strictly preceding subsequent large ruptures. Conversely, we observe weaker, negative anomalies in the footwall, anticorrelated in time with those of the hanging wall, revealing a massive asymmetry in fluid redistribution and permeability evolution across the fault system. Furthermore, aftershock migration rates reveal distinct linear alignments in a distance‐reduced time space, allowing us to explicitly track and quantify episodes of lateral and upward fluid migration. These physically consistent patterns suggest that stress‐driven fluid diffusion directly weakens adjacent fault patches, dictating the spatiotemporal migration of seismicity. We conclude that near‐real‐time monitoring of seismic attenuation may help detect fluid redistribution in active fault systems and may provide useful information for time‐dependent seismic hazard assessment.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 14 May 2026 14:18:15</pubDate>
			<category>Bulletin of the Seismological Society of America</category>
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			<title>Refinement of a framework for Moving Aircraft River Velocimetry (MARV) and application to particle tracking along Alaskan rivers</title>
			<author>Legleiter, Carl; Kinzel, Paul; Laker, Mark; Conaway, Jeff</author>
			<link>https://pubs.usgs.gov/publication/70275694</link>
			<description>&lt;p&gt;&lt;span&gt;Information on river velocities enhances understanding flood hazards, evaluating habitat conditions, and predicting the transport of floating materials. In this follow-up study, we used data from two new sites, one with a more complex morphology and the other with a lower suspended sediment concentration, to provide further evidence that Moving Aircraft River Velocimetry (MARV) can yield accurate velocity estimates ( &lt;i&gt;R&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;/span&gt;&lt;span&gt;&amp;nbsp;up to 0.87 when compared to field measurements) for long segments of large, turbid rivers. The MARV workflow is packaged in freely available software and is robust to implementation details; neither buffering to mitigate edge effects nor a new approach to aggregating velocity vectors improved performance. MARV was not sensitive to parameters used to establish overlapping image sequences, but combining a long window with a short jump between consecutive windows was the optimal configuration. Although accuracy varied from one cross section to the next, agreement between remotely sensed velocities and those measured in the field was independent of position within a frame range. As an initial step toward application of the approach to help address practical problems, we showed how MARV can drive particle tracking models. Our first-order simulations suggest that channel morphology and flow velocity are the primary controls on travel time and particle fate, with diffusive processes playing a lesser role. Although MARV can be used to characterize an instantaneous flow field, a more comprehensive framework that accounts for other physical processes would be required to model specific types of events like oil spills.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Tue, 12 May 2026 13:47:57</pubDate>
			<category>Water Resources Research</category>
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			<title>Simulation of groundwater flow to evaluate hydrogeologic controls on a PFAS plume, Coakley Landfill Superfund site, Rockingham County, New Hampshire</title>
			<author>Harte, Philip; Collins, Andrew</author>
			<link>https://pubs.usgs.gov/publication/sir20265008</link>
			<description>&lt;p&gt;Per- and polyfluoroalkyl substances (PFAS), including perfluorooctanoic acid (PFOA) and perfluorooctanesulfonic acid (PFOS), have been detected at combined concentrations above 2,000 nanograms per liter (ng/L) at groundwater seep locations near the Coakley Landfill Superfund site, in North Hampton, New Hampshire. The landfill was active from 1972 to 1985. An impermeable cap was placed on the landfill in 1998. The adjacent area to the Coakley Landfill has many water supply wells, and transport of PFAS compounds to the wells is a concern. Fracture anisotropy in the underlying bedrock aquifer complicates the understanding of PFAS transport because groundwater preferentially travels along fractures that may not align with the prevailing groundwater flow direction.&lt;/p&gt;&lt;p&gt;In 2018, the U.S. Environmental Protection Agency and the U.S. Geological Survey began an investigation of the groundwater flow from the Coakley Landfill site. This report describes the modification of a numerical groundwater-flow model for the local area around the Coakley Landfill and summarizes findings of the investigation. In addition, this report includes a brief description of PFOA and PFOS occurrence, a discussion of model construction, evaluation of model performance through calibration, and discussion of simulation results for two periods (before and after capping). Limitations are also discussed.&lt;/p&gt;&lt;p&gt;Results show that simulated groundwater flow moves from the Coakley Landfill to the west and north. Advective transport modeling using particle tracking shows that groundwater from the landfill discharges primarily to streams to the west and north, and a small amount is transported to distal wells. Dilution of contaminants through advection and dispersion likely plays a role in whether PFAS compounds from the landfill will be detected above laboratory reporting levels at distal wells.&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 20:03:08</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Walleye In our hands</title>
			<author>Embke, Holly Susan</author>
			<link>https://pubs.usgs.gov/publication/70275700</link>
			<description>&lt;p&gt;No abstract available.&lt;/p&gt;</description>
			<pubDate>Wed, 13 May 2026 13:49:23</pubDate>
			<category></category>
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			<title>Regression models for estimating suspended sediment concentrations and loads and comparison with acoustic surrogate model on the Snake River, Weiser, Idaho, 1977–2022</title>
			<author>Kenworthy, Megan</author>
			<link>https://pubs.usgs.gov/publication/sir20265007</link>
			<description>&lt;p&gt;The U.S. Geological Survey, in cooperation with Idaho Power, developed streamflow- based regression models to estimate suspended sediment concentration (SSC) and loads on the Snake River at Weiser, Idaho site (U.S. Geological Survey streamgage 13269000; hereafter referred to as “Snake at Weiser site”). This site sits upstream from the dams and reservoirs of the Hells Canyon Complex and the Hells Canyon National Recreation Area, where large sandbars along the Snake River that provide recreation and riparian habitat and host archaeological resources have declined since 1973. Analyses of samples from historical (1977- 2003) and modern (2017- 22) periods show that SSC has decreased over time, with median concentrations declining from 50 milligrams per liter (mg/L) to 28 mg/L. Mann- Kendall trend tests confirm statistically significant declines in total SSC and the fine and sand fractions of suspended sediment through the full period of record.&lt;/p&gt;&lt;p&gt;Regression models specific to each period outperformed models using the full dataset, suggesting changes in the sediment supply to this reach of the Snake River and highlighting the need for period- based approaches. Regression models for total SSC and fine sediment were more accurate than those for sand, which exhibited greater error and bias, likely reflecting a sand supply limited by upstream dams. The regression model for modern period total SSC and a previously developed acoustic surrogate model showed similar performance, indicating both methods are viable for estimating SSC and loads.&lt;/p&gt;&lt;p&gt;These findings help to better quantify suspended sediment concentrations and loads upstream of the Hells Canyon Complex and provide resource managers with tools to better quantify sediment loads affecting reservoir storage and the maintenance of sandbars in the Hells Canyon National Recreation Area.&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 17:06:06</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Fossil footprints and Ice Age ecosystems of White Sands National Park</title>
			<author>Springer, Kathleen; Pigati, Jeffrey; Bustos, David; Urban, Thomas; Bennett, Matthew</author>
			<link>https://pubs.usgs.gov/publication/fs20253046</link>
			<description>&lt;h1&gt;Introduction&lt;br&gt;&lt;/h1&gt;&lt;p&gt;In September 2021, National Park Service staff, U.S. Geological Survey scientists, and an international team of researchers revealed evidence in the form of human footprints at White Sands National Park, New Mexico, that showed people were present in North America between 23,000 and 21,000 years ago. This time was during the Last Glacial Maximum, when large ice sheets covered much of the continent. The results stunned the scientific community and sparked a global debate. The story of how the discoveries were made, how they upended traditional thought, and how they “rewrote the book” on the earliest phases of North American prehistory is a classic example of the process of science.&lt;/p&gt;</description>
			<pubDate>Fri, 8 May 2026 14:00:34</pubDate>
			<category>Fact Sheet</category>
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		<item>
			<title>Water use in Louisiana, 2020</title>
			<author>Robinson, Angela</author>
			<link>https://pubs.usgs.gov/publication/sir20265135</link>
			<description>&lt;p&gt;The U.S. Geological Survey (USGS), in cooperation with the Louisiana Department of Transportation and Development, collected water-withdrawal and water-use data from a 2020 inventory of water withdrawals in Louisiana. In 2020, approximately 8,700 million gallons per day (Mgal/d) of water was withdrawn from groundwater and surface-water sources in Louisiana, which represented a 0.22-percent decrease from 2015. Total groundwater withdrawals were about 1,900 Mgal/d, an increase of 7.1 percent from 2015, and total surface-water withdrawals were about 6,800 Mgal/d, a decrease of 2.1 percent from 2015 to 2020.&lt;/p&gt;&lt;p&gt;Total water withdrawals, in million gallons per day, in 2020 for the various categories of use were as follows: public supply, 720; industry, 2,100; power generation, 4,100; rural domestic, 39; livestock, 7.0; rice irrigation, 930; general irrigation, 250; and aquaculture, 590.&amp;nbsp;From 2015 to 2020, Louisiana’s total withdrawals for public supply increased by 1.4 percent, industry decreased by 2.3 percent, power generation decreased by 4.9 percent, rural domestic decreased by 1.2 percent, livestock increased by 11 percent, rice irrigation increased by 13 percent, general irrigation increased by 12 percent, and aquaculture increased by 20 percent.&lt;/p&gt;&lt;p&gt;About 51 percent (approximately 960 Mgal/d) of all groundwater withdrawn was from the Chicot aquifer system and 24 percent (approximately 450 Mgal/d) was withdrawn from the Mississippi River alluvial aquifer. Since 2015, withdrawals from the Chicot aquifer system increased by 13 percent, and withdrawals from the Mississippi River alluvial aquifer increased by 18 percent.&amp;nbsp;About 72 percent (4,900 Mgal/d) of all surface water withdrawn was from the Mississippi River main stem. This value represents a 1.1-percent decrease in withdrawals from 2015 to 2020.&lt;/p&gt;&lt;p&gt;All water-withdrawal and water-use data presented in this report should be considered estimates. Because of rounding, totals and percentages presented in the tables, figures, and text in the report may differ slightly from totals or percentages calculated individually.&lt;br&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 17:02:38</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Riverine pesticide trends in the United States: Assessing a decade of national-scale monitoring</title>
			<author>Shoda, Megan; Breitmeyer, Sara; Hinman, Elise Danica; Stackpoole, Sarah</author>
			<link>https://pubs.usgs.gov/publication/70275677</link>
			<description>&lt;p&gt;&lt;span&gt;Pesticides in freshwater systems can compromise water availability by degrading water quality, with implications for human health and aquatic life. Despite recognition of the need for national-scale monitoring and analysis, few studies have documented long-term trends in surface water pesticide contamination across the US. This study addresses that need by analyzing temporal trends and acute and chronic benchmark exceedances for aquatic life and human health from 81 river sites sampled from 2013 to 2022 using an analytical method targeting 80 pesticides. The majority (79%) of single site and pesticide combinations had too few pesticide detections to estimate trends. When detections were more frequent, increasing trends in concentration were twice as common as decreasing trends. Increasing pesticide concentrations were common in primary drainages of the Mississippi River Basin. Aquatic life benchmarks were exceeded by 19 pesticides, and exceedances were geographically widespread, with both acute and chronic aquatic life benchmark exceedances at 62% of sites. The herbicides atrazine and metolachlor and the insecticide imidacloprid were identified as the greatest threats to surface water availability based on their trends and aquatic life benchmark exceedances. These findings demonstrate the need for continued monitoring and trend analysis, driver investigation, and management strategies to protect freshwater resources.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 14:19:13</pubDate>
			<category>Environmental Science &amp; Technology Water (ES&amp;T Water)</category>
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			<title>Life history traits and population dynamics of Freshwater Drum across large river gradients</title>
			<author>Bouska, Kristen; Solomon, Levi; Bartels, Andrew; DeLain, Steven A.; Gittinger, Eric; Kueter, Travis; Maxson, Kristopher; West, John; Lamer, James; Kim, Hae; Phelps, Quinton</author>
			<link>https://pubs.usgs.gov/publication/70275706</link>
			<description>&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Objective&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;Monitoring and assessment of nongame native fishes is limited, but conservation interest in these species is growing. Freshwater Drum&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Aplodinotus grunniens&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;are a wide-ranging species that serve important functional roles and could serve as an indicator for similar but less common species. Our overall objectives were to quantify and compare population dynamic rates and life history of Freshwater Drum among study reaches in the upper Mississippi and Illinois rivers and relate these metrics to hypothesized environmental and anthropogenic factors.&lt;/p&gt;&lt;/div&gt;&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Methods&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;We integrated recently collected age data with monitoring data to estimate age and size distributions, growth curves, maturation schedules, mortality rates, and young-to-adult ratios of Freshwater Drum in six study reaches spanning 1,500 km of river. Principal component analyses and linear regression were used to relate environmental and anthropogenic gradients (latitude, commercial harvest, hydrologic dynamics, primary productivity) to life history traits and population dynamic rates.&lt;/p&gt;&lt;/div&gt;&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Results&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;We found latitudinal gradients in life history traits and population dynamic rates whereby Freshwater Drum in upstream, higher-latitude study reaches generally exhibited later maturity, slower growth, smaller maximum size, and lower mortality rates compared with those in lower-latitude study reaches. Further, young-to-adult ratios positively corresponded with chlorophyll-&lt;i&gt;a&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;concentration. No clear relationships were apparent between population dynamic rates and hydrologic variation or commercial harvest.&lt;/p&gt;&lt;/div&gt;&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Conclusions&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;Latitude is an important structuring component of life history traits and population dynamics of Freshwater Drum in the upper Mississippi and Illinois rivers likely due to both temperature seasonality and disturbance regimes. The presence of demographic structure in a widespread, common species such as Freshwater Drum suggests similar patterns likely exist in other long-lived native fishes.&lt;/p&gt;&lt;/div&gt;</description>
			<pubDate>Wed, 13 May 2026 14:10:53</pubDate>
			<category>Transactions of the American Fisheries Society</category>
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		<item>
			<title>Los Planes watershed vegetation monitoring: Standard operating procedures</title>
			<author>Wilson, Natalie R.</author>
			<link>https://pubs.usgs.gov/publication/70275684</link>
			<description>This is a description of survey procedures for short term vegetation monitoring at Natural Infrastructure in Dryland Stream (NIDS) structure sites and control sites a ranch in the Los Planes, La Paz, Baja California Sur. This study design was modified from USGS Short Term Vegetation Response Study (Wilson et al. 2021) with the goal to quantify changes in species abundance/cover, structure, and composition. The Society of Ecological Restoration identifies 3 major ecosystem attributes of importance when assessing restoration projects, such as the installation of NIDS (Society for Ecological Restoration International Science &amp; Policy Working Group 2004; Ruiz-Jaen and Mitchell Aide 2005). These attributes are vegetation structure, diversity, and ecological processes. Our protocol can be used to directly quantify vegetation structure and diversity and by collecting data over several years we can indirectly assess the ecohydrological processes associated with NIDS (Norman, Lal, et al. 2022).</description>
			<pubDate>Mon, 11 May 2026 13:48:50</pubDate>
			<category></category>
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			<title>Natomas basin giant gartersnake annual monitoring report 2024</title>
			<author>Nguyen, Allison; Rose, Jonathan; Jordan, Anna C.; Napolitano, Giancarlo; Macias, Daniel; Schoenig, Elliot; Reyes, Gabriel A.; Halstead, Brian</author>
			<link>https://pubs.usgs.gov/publication/ofr20261009</link>
			<description>&lt;p&gt;The giant gartersnake (&lt;i&gt;Thamnophis gigas&lt;/i&gt;) is a semi aquatic snake endemic to the Central Valley of California. After losing 95 percent of its historic wetland habitat (Frayer and others, 1989), giant gartersnakes became state and federally listed as a threatened species (California Fish and Game Commission, 1971; U.S. Fish and Wildlife Service 1993, 1999). Continued monitoring of current populations and implementation of suggested management actions is necessary to recover the species. The Natomas basin in Sacramento, California, supports a population of giant gartersnakes persisting in restored marshes and rice agriculture. This annual report summarizes the giant gartersnake monitoring project for 2024, focusing on the apparent survival, abundance, density, and distribution of the giant gartersnakes and the connectivity of habitat throughout the Natomas basin. In 2024, 131 giant gartersnakes were captured 216 times at 44 sites by hand or trap. The catch-per-unit effort decreased from 2023 to 2024 but was similar to other years of the study. Estimates of occupancy increased between 2023 and 2024, although the trend of occupancy from 2011 through 2024 is still decreasing overall at a mean annual rate of 3 percent per year. Apparent survival was much higher at Betts-Kismat-Silva from 2018 to 2019 and from 2021 to 2022 than in other years, but this may be partly attributed to different sampling efforts over the years. Trapping effort was more consistent in the Sills tract, and apparent survival was slightly higher in later years (2022–23 and 2023–24). Giant gartersnake populations appeared to remain stable in 2024, but abundance, density, survival, and distribution is highly variable across different sites and years of the study. Continued monitoring of the populations would allow for better trend estimates over time and assessment of the effects of management activities. Giant gartersnake populations throughout the basin and on reserve lands would likely benefit from the following: (1) creating more managed marsh; (2) increasing the amount of emergent tule vegetation in existing marshes (for example, Cummings, Natomas Farms, and Lucich South); (3) continuing to flood existing marshes in early spring; (4) maintaining rice agriculture; and (5) continuing research into conservation actions that target the giant gartersnake, such as habitat and water management and translocation.&lt;/p&gt;</description>
			<pubDate>Fri, 8 May 2026 17:28:23</pubDate>
			<category>Open-File Report</category>
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			<title>Assessment of undiscovered oil and gas resources in the Bossier Formation within the onshore United States and State waters of the Gulf Coast Region, 2025</title>
			<author>Gardner, Rand; Birdwell, Justin; Flaum, Jason; Kinney, Scott; Pitman, Janet K.; Paxton, Stanley; Cicero, Andrea; Lagesse, Jenny; Pepin, Jeffrey; Counts, John; Johnson, Benjamin; Lohr, Celeste; Whidden, Katherine; French, Katherine; Mercier, Tracey J.; Leathers-Miller, Heidi M.</author>
			<link>https://pubs.usgs.gov/publication/fs20263004</link>
			<description>&lt;p class=&quot;MsoNormal&quot;&gt;&lt;span&gt;Using a geology-based assessment&amp;nbsp;methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of 3 million barrels of oil&amp;nbsp;and&amp;nbsp;343.5&amp;nbsp;trillion cubic feet of gas&amp;nbsp;in reservoirs of the&amp;nbsp;Bossier Formation&amp;nbsp;within the onshore United States and State waters of the Gulf Coast region.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 17:00:49</pubDate>
			<category>Fact Sheet</category>
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			<title>Inland recreational fisheries harvest far exceeds reported inland harvest in the United States</title>
			<author>Robertson, Matthew; Embke, Holly Susan; Lynch, Abigail; Midway, Stephen; Paukert, Craig</author>
			<link>https://pubs.usgs.gov/publication/70275661</link>
			<description>&lt;p&gt;&lt;span&gt;Recreational fisheries are important global contributors to food security, socio-cultural practices, and local and regional economies. However, inland recreational fisheries are often overlooked by policymakers due to a limited understanding of the magnitude of participation, harvest, and economic impact. Here, we used the U.S. Inland Creel and Angler Survey Catalog and catch and effort model (CreelCatch) and several assumptions to provide an initial estimate of the magnitude of total inland recreational fisheries harvest in the conterminous USA. The CreelCatch model projected fishing harvest across lakes, ponds, and reservoirs based on fishing effort, water body area, and regional effects. We estimated that recreational lake fisheries in the conterminous USA likely harvest 236,000–671,000 tonnes of fish per year, 17–48 times greater than total inland fisheries harvest reported to the United Nations. Inland recreational fisheries may warrant greater consideration for their contribution to national scale socioeconomics and impacts on fish stocks and ecosystems.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 15:11:11</pubDate>
			<category>Fisheries</category>
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			<title>Drift and dispersion of silver carp (Hypophthalmichthys molitrix) eggs and larvae for hypothetical spawning scenarios in the Upper Mississippi River</title>
			<author>LeRoy, Jessica; Loppnow, Grace; Jackson, P.; Lasher, G.</author>
			<link>https://pubs.usgs.gov/publication/70275657</link>
			<description>&lt;p&gt;&lt;span&gt;Invasive carp pose ecological and economic risks to North American freshwater systems. This study uses the Fluvial Egg Drift Simulator to model the drift of invasive silver carp (&lt;/span&gt;&lt;i&gt;Hypophthalmichthys molitrix)&lt;/i&gt;&lt;span&gt;&amp;nbsp;eggs and larvae after hypothetical spawning in Pools 1–10 of the Upper Mississippi River. Although adult invasive carps have been detected in this region, no reproduction has been confirmed as of this publication. A total of 450 spawning scenarios were simulated, representing 5 water temperatures, 9 flows, and 10 spawning locations in the tailwaters of lock and dam structures. The study examined egg and larval positions at two key developmental stages: hatching and gas bladder inflation, when larvae seek nursery habitat. Under a wide variety of flow conditions and water temperatures, eggs spawned upstream from Lake Pepin (Pool 4) are likely to settle in the lake before hatching, possibly increasing mortality rates. Eggs that survive passage through Lake Pepin reach gas bladder inflation within the study area, except in scenarios with lower temperatures and higher flows. Conversely, larvae spawned downstream from Lake Pepin generally drift out of the study area before reaching gas bladder inflation, except in cases of higher temperatures and lower flows. These findings inform ichthyoplankton sampling strategies and management actions aimed at reducing invasive carp populations in areas likely to support recruitment.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 14:43:22</pubDate>
			<category>Scientific Reports</category>
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			<title>Evaluating reservoir passage and survival of juvenile Chinook Salmon to support reintroduction upstream of Shasta Dam, California</title>
			<author>Stockwell, Caitlin; Morse, Joseph; Dirling, Mikaeli; Couch, Claire; Michel, Cyril; Notch, Jeremy; Kock, Tobias J.</author>
			<link>https://pubs.usgs.gov/publication/70275689</link>
			<description>&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Objective&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;Juvenile Chinook Salmon&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Oncorhynchus tshawytscha&lt;/i&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;that are released upstream of Shasta Reservoir migrate more than 35 km to reach Shasta Dam, although survival through this system is poorly understood. We conducted a reservoir-scale acoustic telemetry study to quantify downstream movement and survival under seasonally variable environmental conditions to inform decisions about juvenile collection strategies for Chinook Salmon reintroduction above Shasta Dam.&lt;/p&gt;&lt;/div&gt;&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Methods&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;A total of 656 hatchery-origin juvenile Chinook Salmon were acoustic-tagged, released near the mouth of the McCloud River, and monitored in Shasta Reservoir and the Sacramento River from September 2024 through March 2025 using an array of telemetry receivers.&lt;/p&gt;&lt;/div&gt;&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Results&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;Most tagged fish failed to move downstream through the McCloud River&amp;nbsp;Arm of Shasta Reservoir and arrive at Shasta Dam. Survival probabilities were estimated at 0.268 to the downstream end of the McCloud River&amp;nbsp;Arm and 0.119 to Shasta Dam. For fish that did reach the dam, elapsed time from release to arrival was 66.4 d, and fish typically arrived and departed during daylight hours. Nine tagged juveniles were detected downstream of the dam, and three were later detected more than 500 km downstream.&lt;/p&gt;&lt;/div&gt;&lt;div class=&quot; sec&quot;&gt;&lt;div class=&quot;title&quot;&gt;Conclusions&lt;/div&gt;&lt;p class=&quot;chapter-para&quot;&gt;The consistently low survival and restricted downstream movement provide important information indicating that downstream collection of juvenile Chinook Salmon should be focused in the lower McCloud River and the upper portion of the McCloud River Arm of Shasta Reservoir rather than at Shasta Dam.&lt;/p&gt;&lt;/div&gt;</description>
			<pubDate>Mon, 11 May 2026 14:59:47</pubDate>
			<category>Transactions of the American Fisheries Society</category>
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			<title>Analysis of alternative weir designs for improved passage of select fish at the U.S. Geological Survey streamgaging weir at Blackwells Mills, New Jersey</title>
			<author>Suro, Thomas; Niemoczynski, Michal; Mulligan, Kevin</author>
			<link>https://pubs.usgs.gov/publication/sir20265002</link>
			<description>&lt;p&gt;As the population of New Jersey continues to remain dense, the need for water supply will likely continue to be high, which can lead to water managers needing to make difficult decisions about managing drinking-water supply. Streamgaging weirs like the ones used by the U.S. Geological Survey (USGS) play a critical role in providing accurate and stable streamflow data, but their presence can affect the passage of diadromous fish species such as river herring (&lt;i&gt;Alosa pseudoharengus&lt;/i&gt; [alewife], &lt;i&gt;Alosa aestivalis&lt;/i&gt; [blueback herring], and &lt;i&gt;Alosa sapidissima&lt;/i&gt; [American shad]). In some situations, weirs existing in rivers and streams are no longer used because they were part of a farm irrigation system or some type of industrial operation. The weir at the USGS streamgage 01402000 Millstone River at Blackwells Mills, New Jersey, was purposefully built as a hydraulic-control structure that provides a precise and stable control for the measurement of stage and computation of continuous streamflow. To satisfy the dual need of maintaining accurate streamflow data and providing improved fish passage for select species of fish during migration season, the USGS proposed the development and evaluation of two alternative weir designs that would meet the criteria established for successful passage of American shad, alewife, and blueback herring during their yearly migration. The designs were also required to maintain adequate control of the upstream pool elevation necessary for the precise computation of streamflow used by State agencies for municipal water-supply purposes for surrounding communities.&lt;/p&gt;&lt;p&gt;Two alternative weir design modifications were incorporated at the center of the Blackwells Mills weir and modeled using two-dimensional hydraulic modeling software and three-dimensional computational fluid-dynamics software to simultaneously evaluate conditions for passage of the target fish species and effects to streamflow computations at the streamgage. The models were calibrated to existing conditions around the weir location using surveyed-elevation data and recorded stage, streamflow, and velocity in the Millstone River. The alternative weir designs lowered the weir crest by 1.02 feet (ft) and the resulting simulations showed an effective increase in depth of 0.98 ft at the median streamflow of 251 cubic feet per second (ft&lt;sup&gt;3&lt;/sup&gt;/s) and 0.96 ft at the 95-percent exceedance streamflow of 98 ft&lt;sup&gt;3&lt;/sup&gt;/s. The alternative weir designs were also found to increase streamflow depth across the shallowest portions of the weir structure at the downstream anti-scour skirt by lowering the skirt about 4 inches, allowing for two or more body depths of water for American shad, alewife, and blueback herring at the median migration streamflow of 251 ft&lt;sup&gt;3&lt;/sup&gt;/s. The alternative weir designs also reduced the highest stream velocities across the downstream weir sill and anti-scour skirt from about 9 to 10 feet per second, and the depth-averaged velocity to about 7 to 8 feet per second. The sensitivity of the weir with respect to the computation of streamflow was increased from about 1.8 cubic feet per second per hundredth foot to 1.6 cubic feet per second per hundredth foot for streamflows of about 10–100 cubic feet per second.&lt;/p&gt;</description>
			<pubDate>Mon, 11 May 2026 16:59:37</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Preliminary geologic map of the Sparta East, Sparta West, and parts of the Glade Valley and Whitehead 7.5-minute quadrangles, North Carolina and Virginia, and the epicentral area of the August 9, 2020, Mw 5.1 earthquake near Sparta, North Carolina</title>
			<author>Merschat, Arthur; Carter, Mark; Lynn, Ashley; Weinmann, Benjamin R.; Odom, William; McAleer, Ryan; Mahan, Shannon; Stewart, Kevin; Holm-Denoma, Christopher S.; Crider,, E. Allen</author>
			<link>https://pubs.usgs.gov/publication/ofr20261010</link>
			<description>&lt;h1&gt;Introduction&amp;nbsp;&lt;/h1&gt;&lt;p&gt;New bedrock and surficial geologic mapping in the Sparta East, Sparta West, and parts of the Glade Valley and Whitehead 7.5-minute quadrangles, North Carolina and Virginia, investigates the geologic framework and causative mechanisms of the August 9, 2020, Mw 5.1 earthquake near Sparta, North Carolina. The mapping documents (1) the coseismic surface rupture from the 2020 earthquake and related brittle structures in the bedrock; (2) the fault contact between the western Blue Ridge and eastern Blue Ridge; (3) lithostratigraphy in the Lynchburg Group, Ashe Metamorphic Suite, and Alligator Back Metamorphic Suite; (4) the nature of the contact between the Lynchburg Group, Ashe Metamorphic Suite, and Alligator Back Metamorphic Suite; and (5) surficial deposits.&lt;/p&gt;</description>
			<pubDate>Tue, 5 May 2026 14:00:53</pubDate>
			<category>Open-File Report</category>
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			<title>Regional conservation planning tool: A spreadsheet model to support spatial prioritization and resource allocation decisions</title>
			<author>Couvillon, Anastasia; Soulliere, Gregory J.; Gordon, David H.; Eggeman, Diane; Al-Saffar, Mohammed; Humburg, Dale; Lyons, James E.</author>
			<link>https://pubs.usgs.gov/publication/70275674</link>
			<description>&lt;p&gt;&lt;span&gt;Prioritization is a central component of natural resource management because conservation needs routinely exceed available resources. Waterfowl and wetland conservation programs in North America are at the forefront of landscape-scale prioritization and transboundary management decisions due to the migratory nature of ducks, geese, and swans. The growing availability of geographic information systems (GIS) and geospatial technologies has accelerated the development of multi-objective landscape prioritization models, including applications of structured decision making and multi-criteria decision analysis to spatial planning for waterfowl and wetlands at the continental scale. However, regional managers and conservationists could benefit from flexibility in downscaling continental tools, selecting objectives, and assigning weights for rapid production of spatial prioritization models at smaller spatial scales without extensive computer coding or GIS analysis. We developed a spatial value model that prioritizes landscapes at sub-continental scales (e.g., states and provinces, bird conservation regions, etc.) and provides flexibility for users to select waterfowl conservation objectives of interest and weights. Our model can be used for direct downscaling of an existing continental geospatial model or further customized with region-specific geospatial data. We illustrate how regional prioritization can vary with the spatial scale selected by the user. The spatial value modeling framework and the downscaling tool presented here could increase the use of multi-criteria decision analysis and linear value modeling in spatial landscape prioritization, while also providing flexibility for selecting scales, objectives, and weights. Our spreadsheet tool was developed specifically for use by regional biologists, conservationists, and managers and does not require knowledge of GIS software (although results can be exported from the spreadsheet for spatial analysis using GIS). Together, the model outputs and the accompanying spreadsheet tool provide a bridge between continental waterfowl conservation and regional implementation, enabling rapid, stakeholder-driven, value-explicit prioritization.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 8 May 2026 14:24:23</pubDate>
			<category>Wildlife Society Bulletin</category>
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			<title>Sex-specific Atlantic salmon upstream passage and fallback at a natural cascade after dam removal</title>
			<author>Heim, Kurt C.; Withers, Jonah; Arden, William; Earley, Laurie; Minkoff, David; Castro-Santos, Theodore</author>
			<link>https://pubs.usgs.gov/publication/70275639</link>
			<description>&lt;p&gt;&lt;span&gt;In the Boquet River (NY, USA) a low-head dam set above a ~200-m bedrock cascade was removed in 2015. We used radio-telemetry to assess landlocked Atlantic salmon passage at the remaining cascade (2020, 2022). Across years, 52% of males (13/25) attempted cascade passage whereas females made no discernable attempts (0/11). Attempt probability increased with stream discharge and decreased with fish size, though overall passage success was low (1/36). Shallow depths—likely owing to an artificially widened channel—appear to be limiting passage. Additionally, we transported fish upstream but observed high fallback (72%) that was associated with fish size and energetic status. Following dam removal, this cascade continues to limit upstream passage resulting in increased vulnerability to angling during migratory delay. Overall, we highlight the importance of follow-up studies after dam removal, and that further modifications at this site may be required to improve passage.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Wed, 6 May 2026 14:17:24</pubDate>
			<category>Fisheries Management and Ecology</category>
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			<title>An automated geographic information system-based hydraulic modeling tool for developing preliminary culvert designs for stream crossings in Massachusetts</title>
			<author>Bent, Gardner C.; McCarthy, Brendan; Sturtevant, Luke; McCallister, Meghan; Tudor, Amanda; Armstrong, Ian; Poe, Mark; Graziano, Alexander; Carlson, Carl</author>
			<link>https://pubs.usgs.gov/publication/fs20263065</link>
			<description>&lt;h1&gt;Introduction&lt;/h1&gt;&lt;p&gt;Currently (2026), many of the about 25,000 roadway crossing structures over rivers and streams in Massachusetts are undersized. Undersized culverts and bridges can be detrimental to fish and wildlife movement, habitat continuity, and the health of aquatic organisms. Undersized culverts also can lack the resiliency needed to withstand large floods, which could be worsened by potential increases in flood magnitude and frequency due to climate change. Improving culvert and bridge designs for stream crossing projects may improve aquatic organism passage, stream continuity, and resiliency during future floods by decreasing upstream overbank flooding, road flooding and erosion, and degradation of aquatic habitat.&lt;/p&gt;&lt;p&gt;The U.S. Geological Survey (USGS), Massachusetts Department of Environmental Protection (MassDEP), and University of Massachusetts Amherst began a series of cooperative studies in July 2019 to develop an automated geographic information system (GIS) hydraulic modeling tool for preliminary culvert designs for stream crossings. The USGS plans to provide preliminary culvert designs in the web-based StreamStats application, which enables municipalities and engineers to view potential designs and related information for stream crossing replacement projects in Massachusetts. This application can (a) provide information on hydrology, hydraulics, and ecological conditions at stream crossing sites, (b) provide users with potential culvert designs to improve aquatic organism passage and flood resiliency, and (c) assist MassDEP in implementing the Massachusetts Wetlands Protection Act regulations for stream crossing projects.&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 19:08:48</pubDate>
			<category>Fact Sheet</category>
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			<title>An overview and participatory framework for choosing spatial boundaries in social–ecological systems modeling</title>
			<author>Perella, Christina; Vukomanovic, Jelena; Hickman, Caleb R.; Terando, Adam; Eaton, Mitchell; Schaefer, Marie</author>
			<link>https://pubs.usgs.gov/publication/70275653</link>
			<description>&lt;p&gt;&lt;span&gt;A common challenge when modeling social–ecological systems (SESs) is defining the spatial extent of the system. Boundaries that do not adequately capture both social and ecological processes and their interactions can lead to mischaracterization of the system, while expanding boundaries too widely can impact model complexity and required resources. Socially, boundaries can invoke and influence identity, culture, power, and sense of place. Boundary decisions benefit from flexible, iterative approaches and the expertise of local communities. Here, we use a structured database search supplemented with citation searching to identify and review the literature that addresses choosing or defining spatial boundaries in SESs mapping or modeling and, when applicable, how participatory methods were used in the research process. In a review of the resulting 79 studies, we discovered that pre-existing social or ecological boundaries were used most frequently (36 and 18 publications, respectively). Twenty-one publications combined social and ecological boundaries or data to create custom boundaries, and four studies used an alternative approach to conventional boundaries. Informed by the literature review, we present a general framework for defining boundaries at the outset of SES research. We then connect the framework to a specific case study based on a collaborative project with Tribal, university, and federal scientists to develop a social–ecological climate adaptation plan. We present guiding questions alongside candidate boundaries for our study system and explore the tradeoffs of these boundary options, which can function as a useful template for other social–ecological research collaborations.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 15:15:49</pubDate>
			<category>ISPRS International Journal of Geo-Information</category>
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			<title>The United States Magnetotelluric Array and the National Impedance Map</title>
			<author>Kelbert, Anna; Bedrosian, Paul; Schultz, Adam; Egbert, Gary; Pellerin, Louise; Love, Jeffrey; Frassetto, Andy; Murphy, Benjamin S.</author>
			<link>https://pubs.usgs.gov/publication/70274338</link>
			<description>&lt;p&gt;&lt;span&gt;The United States Magnetotelluric Array (USMTArray) data set, collected in the years 2006–2024, consists of more than 1,700 long-period magnetotelluric stations covering the entirety of the contiguous United States on a quasi-regular 70&amp;nbsp;km grid. Funding across multiple federal agencies was critical to sustaining this effort to its completion. Important components of the project included active guidance and participation from the MT community, the open and timely availability of all data, and the application of consistent instrumentation and robust data processing. Together with parallel advancement in the development of publicly available three-dimensional (3D) inversion codes, the USMTArray has revitalized the US magnetotelluric community and increased the visibility of magnetotellurics within the Earth-science community. Taken as a whole, these data are visualized as the National Impedance Map, which, together with a 3D synthesis conductivity model of the nation, reveals the electrical architecture of the contiguous US. USMTArray data are used by researchers worldwide for fundamental and applied studies, including investigations of continental architecture and evolution, estimation of hazards to critical infrastructure due to geomagnetic storms, and assessment of the nation&apos;s undiscovered geothermal and mineral resources. We here review the history and development of the project, discuss the challenges and successes in its execution, present the National Impedance Map and synthesis conductivity model, and highlight the breadth of research stemming from this rich data set.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 14:26:55</pubDate>
			<category>Reviews of Geophysics</category>
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			<title>Understanding the occurrence and distribution of per- and polyfluoroalkyl substances (PFAS) in surface waters of the nontidal Passaic River Basin</title>
			<author>Schreiner, Molly L.; Romanok, Kristin; Gray, Jacob; Brown, Eileen; Williams, Brianna; Kneser, Maureen; Capuzzi, Albert; Boerner, Jason; Giunta, Luke; Serillo, Paul; Trainor, John; Smalling, Kelly</author>
			<link>https://pubs.usgs.gov/publication/sir20265018</link>
			<description>&lt;p&gt;This study, completed by the U.S. Geological Survey in cooperation with the North Jersey District Water Supply Commission (NJDWSC), was designed to characterize the occurrence and distribution of per- and polyfluoroalkyl substances (PFAS) in surface waters of the nontidal Passaic River Basin in New Jersey that have the potential to affect public-drinking-water quality. In 2025, 37 sites in the Wanaque, Ramapo, Pompton, and Passaic River watersheds were sampled in January, March, July, and September under base-flow conditions and a subset of sites was sampled during two rain events. Samples were analyzed for 40 individual PFAS and total organic carbon and a subset of samples was analyzed for 1,4-dioxane and trace elements. Fifteen PFAS were detected at least once, with individual concentrations ranging from 0.42 to 28 nanograms per liter (ng/L; median, 2.8 ng/L). Perfluorooctanoate (PFOA) and perfluorooctane sulfonate (PFOS) were widespread and detected in 100 and 97 percent of the samples, respectively. Concentrations of PFOA and PFOS ranged from 1.2 to 28 ng/L (median, 7.7 ng/L) and from 0.52 to 12 ng/L (median, 3.8 ng/L), respectively. Generally, concentrations were lower in the Wanaque and Ramapo River watersheds compared to the Pompton and Passaic River watersheds. Concentrations of PFOA and PFOS were highest in July and September when flows were low. During rain events, median concentrations of PFOS were elevated compared to those observed under base-flow conditions, indicating potential inputs from non-point sources. To understand potential drivers of PFAS concentrations, land cover and potential PFAS sources were summarized for each sampling site, and an accumulated wastewater model was used to estimate the percentage of wastewater from upstream municipal and industrial sources in all flowlines of the Passaic River Basin. Developed land, the number of potential sources, and the mean-annual accumulated wastewater percentage were highly correlated with PFAS concentrations and Deciduous Forests were negatively related to concentrations. Data provided by this study can be used by water purveyors and resource managers to make treatment and mitigation decisions to minimize PFAS in local surface waters used as drinking-water resources.&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 16:47:30</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Assessment of long-term trends in streamflow statistics within and near the Mobile Bay and Perdido Bay watersheds, United States, 1950–2022</title>
			<author>Asquith, William; Crowley-Ornelas, Elena; Whaling, Amanda</author>
			<link>https://pubs.usgs.gov/publication/sir20265142</link>
			<description>&lt;p&gt;The U.S. Geological Survey, in cooperation with the Gulf Coast Ecosystem Restoration Council, assessed monotonic trends for a variety of streamflow statistics for 69 long-term U.S. Geological Survey streamgages within either the Mobile Bay or Perdido Bay watersheds that were active through at least at the end of calendar year 2019. Long-term data were defined for this investigation as having at least 50 years of cumulative record within the period since January 1, 1950, with a requirement for a complete record of streamflow during the 2010s (2010–19). The 69 streamgages have at least 54 years and as many as 73 years of daily mean streamflow data; the median period of record is 72 years; and 15 of the streamgages are identified as “major nodes” on the basis of the criteria described. The occurrence of statistically monotonic significant trends for the 69 streamgages at the 0.05 significance level is spatially shown for six statistics. For the major node streamgages, the study depicts (1) time-series graphics of annual mean, annual harmonic mean, decadal 10th, 50th, and 90th-percentile streamflows, and (2) a variation on Quantile-Kendall plots of Kendall’s tau and streamflow nonexceedance probabilities for each of the 365 days of a year. Trend assessment synthesis shows that, except for a few streamgages with relatively greater counts of statistically significant trends than others, the majority (about 93 percent) of individual trend tests indicate no trend in the streamflow and ecological metrics considered.&lt;br&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 16:45:34</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Building resilience in dryland ecosystems: A climate adaptation strategy menu for pinyon–juniper woodlands</title>
			<author>Gray, Jesse; Slate, Mandy; Ennis, Alyson; Peterson, Courtney; Bradford, John B.; Noel, Adam; Duniway, Michael; Bishop, Tara; Barrett, Ian; Domschke, Chris; Humphries, Joel; Barger, Nicole</author>
			<link>https://pubs.usgs.gov/publication/70275589</link>
			<description>&lt;p&gt;&lt;span&gt;Pinyon–juniper (PJ) woodlands, one of the most extensive mature and old-growth woodland types in the Western United States, provide critical ecological, cultural, and economic benefits but face increasing threats from climate change, altered disturbance regimes, invasive species, and pests. We developed the PJ Woodland Climate Adaptation Management Menu, a decision support tool designed to guide adaptive, climate-informed management of PJ ecosystems, particularly within the Colorado Plateau ecoregion. The menu was created through an iterative, collaborative process involving literature review, integration of strategies from existing adaptation frameworks, and extensive input from scientists, land managers, and community partners during workshops and focus groups. The menu links specific, evidence-based approaches to each of six broad strategies, including soliciting community input, mitigating disturbance, enhancing and maintaining biodiversity, conserving ecotones, timing actions for optimal outcomes, and accepting climate-driven changes when appropriate. It is intended for use with the Adaptation Workbook to help managers connect local goals and climate vulnerabilities to tailored management tactics. Hypothetical scenarios demonstrate the menu’s application to contrasting PJ woodland conditions, from die-off events to old-growth maintenance. Lessons learned during development underscore the value of early stakeholder engagement, cross-sector collaboration, and balancing diverse ecological objectives. This menu offers a flexible, transferable framework to strengthen climate resilience in PJ woodlands and serves as a model that could improve adaptation planning in other dryland forest ecosystems.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 4 May 2026 14:55:50</pubDate>
			<category>Forests</category>
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			<title>Nest site and habitat changes over 15 years in a predicted climate refugium in Beluga, AK, USA, have a positive impact on Hudsonian godwit (Limosa haemastica) nest survival</title>
			<author>Smith, Eden; Swift, Rose; Courtemanche, Anna; Huang, Feipeng; Pelton, Mary; Puleo, Lauren; Simmonds, Josiah; Waller, Matthew; Walton, Hannah; Weissburg, Casey; Wilde, Luke; Senner, Nathan</author>
			<link>https://pubs.usgs.gov/publication/70275662</link>
			<description>&lt;p&gt;&lt;span&gt;Climate change is transforming the Arctic and sub-Arctic at a pace that threatens many taxa with population declines and extinction. However, some habitats–such as muskeg bogs–can serve as climatic refugia and lessen the effects of a changing climate on the species that rely on them. Hudsonian Godwits (&lt;/span&gt;&lt;i&gt;Limosa haemastica&lt;/i&gt;&lt;span&gt;) are a species of migratory shorebird that utilizes the muskeg bogs of Alaska and Canada to breed. Our study focused on a muskeg bog in Beluga, Alaska, USA to see if it had changed from 2009 to 2023, if the availability of Godwit nests sites in the bogs changed in concert, and if Godwit nest survival was affected by any of these changes. We found that, overall, the bog dried and became more vegetated, with the proportional cover of graminoids, shrubs, and forbs all increasing during our study. Godwit nest sites also changed, with the proportion of shrubs and graminoids around nests increasing over time. Nonetheless, these changes did not negatively impact Godwit nest survival. Instead, nest survival increased ~ 22% during our study period, and we observed no decline in the number of potential nests sites available to Godwits. Taken together, these results suggest that while muskeg bogs are changing, they are also currently acting as climate refugia for Godwits. However, it is unclear for how long muskeg bogs can continue to buffer Godwits and other species from the effects of climate change.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 14:50:17</pubDate>
			<category>Polar Biology</category>
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			<title>Evaluating approximations of river channel shape using a national cross section database</title>
			<author>Legleiter, Carl; Kinzel, Paul</author>
			<link>https://pubs.usgs.gov/publication/70275370</link>
			<description>&lt;p&gt;&lt;span&gt;Many hydrologic applications require basic information on the size and shape of river channels, but measuring cross section (XS) geometry in the field or via remote sensing can be costly and often provides only partial coverage. Given these challenges, we capitalized upon an existing data set of 46,971 XS from gaging stations to evaluate various approximations of channel shape. After screening and pre-processing these data, we fit four model types to each XS, including a new approach that involves Stacking PDFs (probability density functions) to Approximate River Channel Shapes (SPARCS). This framework produced depth estimates that closely matched field measurements, with typical cross-sectional area errors &amp;lt;1&lt;/span&gt;&lt;span&gt;% and a median &lt;i&gt;R&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;/span&gt;&lt;span&gt;&amp;nbsp;of 0.77 for comparison of observed and predicted depths. SPARCS model parameters can be interpreted in terms of channel characteristics: mean depth, asymmetry, bar convexity, and flatness of the bed. The model performed well for the XS included in the database, which was biased toward straight, uniform channels conducive to operational streamflow measurement. Neither model parameters nor accuracy were dependent on discharge. We also assessed the potential of SPARCS to fill in measurement gaps and found that although the model can help, the accuracy of inferred depths decreased as the observable fraction of the channel decreased. An important limitation of SPARCS is that mid-channel bars or multi-threaded morphologies cannot be produced. Graphical tools can help visualize how model parameters affect simulated river forms. SPARCS could facilitate satellite-based discharge estimation by providing prior information on channel shape.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 14:00:47</pubDate>
			<category>Water Resources Research</category>
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			<title>Changes in suspended sediment concentration along tidal rivers of the Chesapeake Bay: The tidal freshwater “sediment shadow”</title>
			<author>Noe, Gregory; Murphy, Rebecca; Krauss, Ken</author>
			<link>https://pubs.usgs.gov/publication/70275718</link>
			<description>&lt;p&gt;&lt;span&gt;Transport of terrigenic sediment from nontidal watersheds into estuaries has important impacts on coastal habitat quality, pollutant transport, and resilience to sea-level rise. However, relatively little is known about changes in suspended sediment as nontidal rivers encounter tide, transition into tidal rivers through the tidal freshwater zone (TFZ), and enter saline portions of estuaries. The goal of this paper is to identify spatial and temporal patterns in suspended sediment concentration (SS) changes across tidal and salinity gradients over multiple tidal rivers, using a robust monitoring long-term dataset from the Chesapeake Bay. The multiple TFZs in the Chesapeake Bay consistently have a “sediment shadow” shown by a local spatial minimum in SS compared to upstream nontidal and downgradient oligohaline river reaches. Similarly, freshwater inputs from nontidal rivers have diminishing influence on tidal SS temporal dynamics with distance downstream from the head-of-tide. Therefore, little of the contemporary watershed sediment load is likely transported past the TFZ except during extreme floods when some sediment may be delivered to saline portions of the estuary. Tidal freshwater and brackish portions of the estuary have spatially variable trends in SS over time, both increases and decreases. However, the more saline downstream ends of tidal rivers and the mainstem of the Chesapeake Bay have had a consistent average 25% decline in SS over the past decades. In summary, the presence of “sediment shadows” suggests watershed loads of sediment are currently mostly not transported through the TFZ into the saline estuary, and likely generate sediment deficits for tidal freshwater wetlands.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 13:15:07</pubDate>
			<category>Estuarine, Coastal and Shelf Science</category>
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			<title>Socio-ecological impacts of the 2025 Los Angeles urban fires on communities, neighborhoods, and homes</title>
			<author>Norlen, Carl; Sharma, Sadikshya; Escobedo, Francisco</author>
			<link>https://pubs.usgs.gov/publication/70275365</link>
			<description>&lt;p&gt;&lt;span&gt;Human settlements are increasingly being impacted by urban fires initiated by wildfires. Metrics such as area burned and number of structures destroyed are important, but research often overlooks the socio-ecological complexity of urban fires. We study the impacts of the 2025 Los Angeles fires on two communities at the neighborhood and residential parcel scales. Geospatial analyses and econometric modeling explore the relationships between urban morphology, socio-demographic factors, and home destruction. Here we show that socio-ecological characteristics and scale are key in parsing the dynamics of urban fires. Also, new socio-demographic populations are being affected and urban morphology metrics are more important than vegetation cover. Despite parallels with 19&lt;/span&gt;&lt;sup&gt;th&lt;/sup&gt;&lt;span&gt;&amp;nbsp;and early 20&lt;/span&gt;&lt;sup&gt;th&lt;/sup&gt;&lt;span&gt;&amp;nbsp;century urban conflagrations, understanding these re-emerging urban fires requires transdisciplinary approaches and unique metrics. Investigating the socio-ecological scales and dynamics of urban fires provides a valuable next step towards understanding and adapting to the risk associated with these disasters.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 14:59:05</pubDate>
			<category>Nature Communications</category>
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			<title>Hydrologic investigation of water level fluctuations at Moreau Lake, Moreau Lake State Park, town of Moreau, New York</title>
			<author>Heisig, Paul M.</author>
			<link>https://pubs.usgs.gov/publication/sir20265132</link>
			<description>&lt;p&gt;The causes of water level fluctuations at Moreau Lake, within Moreau Lake State Park in the town of Moreau, New York, were investigated from 2016 to 2021 after lake water levels dropped between 2015 and 2016, raising concerns about the loss of a shallow swimming area at the park beach. Annual variation in precipitation records from the area did not account for the lake water level decline. Two possible causes for the low lake water levels were investigated: the increase in groundwater withdrawals from new residential development since about 2000 and seasonal changes (nongrowing and growing seasons) in precipitation.&lt;/p&gt;&lt;p&gt;Investigation of the potential effects of nearby groundwater withdrawals required the compilation and collection of well-log data, seismic surveys, and measurements of lake and groundwater levels, field chemical parameters, and water isotopes to define the hydrogeologic system and to estimate water use. The net result of this work was the determination that Moreau Lake is a “flow though” lake with no surface water outlet; groundwater enters the lake on the upgradient side and exits through the downgradient side, however, groundwater does not flow southward from the lake toward nearby groundwater withdrawals from the semiconfined aquifer, and thus groundwater withdrawals were unlikely to have an effect on lake water levels.&lt;/p&gt;&lt;p&gt;Investigation of the historic precipitation records during nongrowing (November through April) and growing (May through October) indicated that (1) nongrowing season precipitation from 2011–12 to 2015–16 was more deficient than any similar period during the past 78 years and (2) since about 2000, nongrowing seasons have been drier overall and growing seasons have been considerably wetter. Initiation of lake water level monitoring in 2016 provided an opportunity to compare seasonal precipitation with seasonal lake water level changes. Nongrowing season lake water levels are very sensitive to precipitation, such that high precipitation (40 percent above the seasonal median) resulted in a 5-foot rise in lake water level. In contrast, the growing season lake water levels are sensitive to dry conditions; for example, deficient rainfall (about 6 percent below the seasonal median) resulted in a decline of lake water levels of about 3.5 feet. However, lake water levels are insensitive to high growing season rainfall inputs (about 10 to 47 percent above the seasonal median); lake water levels consistently declined about by 0.8 feet above this range of seasonal excessive precipitation.&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 16:44:17</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>A hierarchical approach for finding undiscovered populations of an endangered bumble bee</title>
			<author>Otto, Clint; Schrage, Alma; Lothspeich, Audrey Claire; Bailey, Larissa L.; Smith, Tamara; Planman, Robert; Cardin, Judy; Ellis, Kristen; Dennis, Bethany; Grundel, Ralph</author>
			<link>https://pubs.usgs.gov/publication/70275646</link>
			<description>&lt;p&gt;&lt;span&gt;Understanding the distributions of rare species is necessary to guide monitoring and inform species recovery efforts. The rusty patched bumble bee (RPBB;&amp;nbsp;&lt;/span&gt;&lt;i&gt;Bombus affinis,&lt;/i&gt;&lt;span&gt;&amp;nbsp;Cresson) is an endangered species with an extant, known distribution centered around urban areas of the Midwestern United States. We tested a novel approach for finding undocumented RPBBs outside of urban centers and estimated the species occurrence at two scales that are relevant to management. We confirmed presence of RPBBs at 54% of the sampled 100 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;grid cells where the species was previously undocumented, expanding the species’ known distribution by 5700 km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;. After accounting for imperfect detection, our occupancy model estimated the number of occupied grid cells was 67 of 105 sampled grids, suggesting our methods were effective for finding undiscovered RPBB sites. Occupancy within 100&amp;nbsp;km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;grids was positively related to the number of occupied neighboring units but was not related to the area of developed land within 100km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;&amp;nbsp;grid cells or smaller subunits (i.e. 3.14&amp;nbsp;ha patches or roadside transects). We highlight the utility of our approach for guiding future survey efforts by identifying an additional 145 grid cells where the occupancy status of RPBB is unknown but we predict a relatively high likelihood of RPBB occurrence. Our approach can be extended to find undiscovered RPBB sites in other areas and applied to other bee species where occurrence information is lacking outside of their core distribution.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 15:00:45</pubDate>
			<category>Scientific Reports</category>
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			<title>Shallow hydrogeologic framework of the Tully Valley mudboil area, Onondaga County, New York</title>
			<author>Williams, John; Terry, Neil; Kappel, William; Heisig, Paul M.; Glas, Robin; Woda, Joshua</author>
			<link>https://pubs.usgs.gov/publication/sir20265129</link>
			<description>&lt;p&gt;&lt;span&gt;Mudboils have been documented in the Tully Valley in southern Onondaga County, New York, since the late 1890s. Sediment-laden water from the mudboils flows into Onondaga Creek, which empties into Onondaga Lake at Syracuse 15 miles to the north. Turbidity from the mudboils has degraded the water quality of Onondaga Creek despite a series of mitigation efforts that began in the early 1990s. Turbidity mitigation actions presently (2025) being considered include creek relocation and offline sediment settling. In support of these proposed actions during 2021–23, the U.S. Geological Survey, in cooperation with the New York State Department of Environmental Conservation, U.S. Environmental Protection Agency, Onondaga Nation, Onondaga Environmental Institute, and Central New York Regional Planning and Development Board, collected and analyzed geologic, hydrologic, geophysical, and geotechnical data to characterize the shallow hydrogeology along four proposed creek-relocation paths and in the proposed offline settling basin area.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;The investigation indicated that the four proposed creek-relocation paths, two east of Onondaga Creek and two west of Onondaga Creek, are underlain by sediments including muck, alluvium, mudboil deposits, alluvial-fan sand and gravel, and lacustrine fines. The proposed excavations would penetrate partially to fully saturated conditions: generally, the water table is shallow near the creek and deep on the alluvial fans. The shallowest excavation, about 5 feet below land surface, would be near the creek and primarily in alluvium, and the deepest excavation, as much as 30 feet below land surface, would be in the alluvial-fan deposits. Brackish waters would be penetrated by proposed channel excavations on the eastern side of Onondaga Creek in an area downgradient from a potentially leaking historical salt-exploration borehole and near the main mudboil area. Excavation in these areas likely would provide a continuous source of brackish groundwater to the relocated creek. Proposed channel excavations of muck, soft to very soft lacustrine fines, and mudboil-type sediments in mudboil and suspected mudboil areas would pose an excavation and slope stability challenge and would have the greatest potential to create new mudboils. Proposed channel excavations below the water table on the Rattlesnake Gulf and Rainbow Creek alluvial fans would intercept groundwater and make the constructed streambank susceptible to seepage-induced slope instability. The substantial water-level fluctuation in the sediments of both alluvial fans would aggravate the stability condition. In addition, excavation on the Rattlesnake Gulf alluvial fan would have the potential to affect water-supply springs at the toe of the fan.&lt;/p&gt;&lt;p&gt;The proposed offline settling basin area is in the northern part of the Rattlesnake Gulf alluvial fan. Natural and man-made diversions of Rattlesnake Gulf have resulted in saturated conditions in the general area of the proposed basin. The proposed offline settling basin would be excavated in, and berms would be constructed on, alluvial-fan deposits and lacustrine fines. In the proposed basin area, the alluvial deposits overlying the lacustrine fines are less than 10 feet thick. Excavation, berm construction, and loading of the saturated, soft to very soft lacustrine fines may be problematic and require soil strengthening.&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 16:42:15</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Springtime formation of laminated soil carbonate rinds and changes in fluvial terrace soils on orbital timescales at Rio Mesa, Utah, USA</title>
			<author>Huth, Tyler; Cerling, Thure; Marchetti, David; Ellwein, Amy; Mahan, Shannon; Bowling, David; Passey, Benjamin; Polyak, Victor; Asmerom, Yemane</author>
			<link>https://pubs.usgs.gov/publication/70275353</link>
			<description>&lt;p&gt;&lt;span&gt;Laminated soil carbonate rinds are a Quaternary paleoclimate archive whose isotope composition is linked to soil formation conditions. At Rio Mesa, Utah (USA), we investigated the fidelity of rind records in a river terrace setting by determining the seasonal timing of rind formation and testing for inter-record replication. We infer soil carbonate formed in the spring season, contrasting with our prior inference of summer formation at Teasdale, Utah, ≈200&amp;nbsp;km distant. This apparent discrepancy occurs because of differences in the timing of the largest annual infiltration (spring vs. summer). At Rio Mesa, modern soil data show that soil carbonate δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C would have high values (−2 to 2‰ VPDB) regardless of seasonal activity of C&lt;/span&gt;&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;versus C&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;plants because respiration rate is a strong control. We accordingly suggest reassessment of published records interpreting soil carbonate δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C only via C&lt;/span&gt;&lt;sub&gt;3&lt;/sub&gt;&lt;span&gt;&amp;nbsp;versus C&lt;/span&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;span&gt;&amp;nbsp;plant abundance. Three rind δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C and δ&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O records generally replicated. Intriguingly, rind δ&lt;/span&gt;&lt;sup&gt;13&lt;/sup&gt;&lt;span&gt;C may inversely correlate with summer insolation, evidence for global-scale influence on soils. Rind δ&lt;/span&gt;&lt;sup&gt;18&lt;/sup&gt;&lt;span&gt;O is not as clearly correlated with published western USA paleoclimate records, potentially due to regional differences in climate and because rinds record soil-specific processes. Our results support the fidelity of the soil carbonate rind paleoarchive and suggest that because rind formation seasonality is intimately tied to infiltration seasonality, spatial transects of rind records might be used to delineate boundaries between areas dominated by spring and summer infiltration, permitting reconstruction of the geographic extent of large-scale hydrologic phenomena such as the North American Monsoon.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 13:21:06</pubDate>
			<category>Geochemistry, Geophysics, Geosystems</category>
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			<title>Modeling chronic wasting disease transmission risk in mule deer related to habitat characteristics</title>
			<author>Christensen, Erica; Kleist, Nathan; Edmunds, David; Heinrichs, Julie A.; Saher, D. Joanne; Whipple, Ashley; DeVivo, Melia; Aldridge, Cameron</author>
			<link>https://pubs.usgs.gov/publication/70275363</link>
			<description>Chronic wasting disease (CWD) is a prion disease of cervids that spreads to uninfected individuals through direct transmission (contact with infected individuals), vertical transmission (from mother to offspring), or indirect transmission (exposure to contaminated environments). The risk of indirect transmission is unevenly distributed on the landscape, and risk levels are expected to be controlled by patterns of habitat use by infected and uninfected individuals as well as environmental properties that alter the length of time prions remain infectious and available for uptake. Despite evidence from controlled or laboratory studies identifying environmental properties likely to affect patterns of CWD prion locations on the landscape, it remains difficult to connect mechanisms to realized increased or decreased risk of disease transmission, and few studies have attempted to detect patterns of different CWD risk in different environments. Using data from GPS-collared mule deer in Wyoming that were CWD-tested annually, we constructed models predicting annual probability of disease transmission contingent on environmental properties extracted from GPS use points. We compared models that emphasized different pathways of disease transmission by including or excluding sets of covariates that described deer density, habitat selection, and covariates expected to affect prion persistence in the environment. Results indicated that key habitat characteristics often selected by mule deer, such as proximity to secondary roads, were also associated with higher risk of testing positive for CWD, which supports the hypothesis that disease risk was correlated to patterns of habitat use by deer. We also found increased risk associated with spatial properties that were not selected-for by deer, such as areas where topography collects moisture, suggesting that prion retention mechanisms also play a role in risk. Incorporating these spatially-varying risk factors into our understanding of CWD transmission and outbreak progression can support managers in designing data collection and disease management strategies.</description>
			<pubDate>Fri, 1 May 2026 13:56:46</pubDate>
			<category>PLoS ONE</category>
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			<title>Asynchronous landslide seasonality across the United States</title>
			<author>Luna, Lisa Victoria; Mirus, Benjamin; Collins, Brian; Perkins, Jonathan</author>
			<link>https://pubs.usgs.gov/publication/70275643</link>
			<description>&lt;p&gt;&lt;span id=&quot;_mce_caret&quot; data-mce-bogus=&quot;1&quot; data-mce-type=&quot;format-caret&quot;&gt;&lt;span&gt;Mid-range landslide outlooks can facilitate weather-related landslide preparedness and disaster response planning, but seasonal landslide activity remains poorly quantified at continental scales. Leveraging &amp;gt;55,000 reported landslides from across the United States (U.S.), we used circular statistics to quantify landslide seasonality in 67 National Weather Service County Warning Areas (CWAs). We found regional differences in landslide season timing and duration, with transitions between domains variably corresponding to climate class or river basin. We assessed differences in seasonality by movement type for slides, flows, and falls, detecting apparent, but uncertain, differences between slide and fall seasonalities in 27 of 35 (77%) of CWAs with both types reported. In the Pacific Northwest, where long records exist, we found a credible shift toward a later mean landslide season in western Washington from 1990 to 2020, but no trend in western Oregon. Our results can provide emergency planners a resource to assess seasonal landslide probability nationwide.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 15:15:20</pubDate>
			<category>Geophysical Research Letters</category>
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		<item>
			<title>Yellowstone grizzly bear investigations 2024: Annual report of the Interagency Grizzly Bear Study Team</title>
			<author></author>
			<link>https://pubs.usgs.gov/publication/70275669</link>
			<description>&lt;p&gt;No abstract available.&lt;/p&gt;</description>
			<pubDate>Fri, 8 May 2026 15:04:06</pubDate>
			<category>Annual Report</category>
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			<title>Characterizing the long-term (1981–2023) temperature and precipitation dynamics in the Trans-Mountain regions of Kazakhstan, Central Asia</title>
			<author>Duisebek, Baktybek; Senay, Gabriel; Usmanov, Talgat; Kyrgyzbay, Kudaibergen; Sagin, Janay; Mukanov, Yerbolat; Samarkhanov, Kanat; Wang, Xuejia; Danierhan, Sulitan; Pan, Xiaohui</author>
			<link>https://pubs.usgs.gov/publication/70275326</link>
			<description>&lt;p&gt;&lt;span&gt;Mountain regions are highly climate-sensitive, yet long-term observational evidence of elevation and seasonal climate dynamics in Central Asia remains limited. This study examines spatiotemporal trends in temperature (Tmean, Tmax, Tmin, and diurnal temperature range [DTR]) and precipitation across Kazakhstan’s transmountain regions using 74 meteorological stations (1981–2023). Data were analyzed using the Mann–Kendall test and Sen’s slope estimator, stratified across six elevation zones from lowlands (&amp;lt;400 m) to high mountains (&amp;gt;1500 m). Results reveal a robust, spatially coherent warming signal across all zones. Annual Tmean increased at a median rate of ~0.30 °C decade&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;, peaking at 0.36 °C decade&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;above 1500 m, corresponding to an absolute increase exceeding 1.5 °C. Warming exhibited strong seasonal and diurnal asymmetries. Spring warmed most rapidly, with Tmean increasing &amp;gt;0.60 °C decade&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;&amp;nbsp;(approaching 3 °C total). Winter warming was driven by Tmin increases (up to 0.44 °C decade&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;), causing widespread DTR contraction, whereas summer warming was driven by Tmax increases, expanding DTR at higher elevations. Tmin showed the strongest elevation amplification overall. In stark contrast, precipitation trends were weak, spatially heterogeneous, and largely non-significant. Annual changes ranged from −6.63 to +14.35 mm decade&lt;/span&gt;&lt;sup&gt;−1&lt;/sup&gt;&lt;span&gt;, with seasonal tendencies indicating modest, non-significant winter/spring wetting and summer drying. Ultimately, the results demonstrate a profound decoupling between strong, elevation-dependent warming and weak precipitation changes. The acute amplification of temperature, particularly during spring and summer at high elevations, has severe implications for snowmelt timing, glacier mass balance, evapotranspiration demand, and long-term water security in Kazakhstan.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Wed, 29 Apr 2026 14:27:38</pubDate>
			<category>Water</category>
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			<title>Using structured decision-making to develop a communications strategy for the U.S. Geological Survey Cooperative Research Units Program</title>
			<author>Robinson, Kelly; Sells, Sarah; McGowan, Conor; Irwin, Elise</author>
			<link>https://pubs.usgs.gov/publication/70275316</link>
			<description>Communication regarding the mission of the U.S. Geological Survey (USGS) Cooperative Research Units Program (CRU) can take many forms, yet clear and concise messaging for various audiences is critical to highlight program accomplishments and increase visibility. Before the work described in this report, CRU did not have a communication strategy; therefore, CRU leadership supported a structured decision-making (SDM) workshop to develop a comprehensive strategy for multiple audiences. The workshop was conducted in November 2024, in Nebraska City, Nebraska. The working group for this SDM process included CRU Program leadership, the CRU Communications Team lead, Unit scientists, a Unit administrative assistant, a representative of the Wildlife Management Institute (WMI), a member of the USGS Ecosystems Mission Area (EMA), Office of Communications and Publishing (OCAP) team, and the team lead for the CRU Program strategic planning process, as well as three facilitators who were also unit scientists as well as experts in SDM. Over the course of a week, the SDM team followed the PrOACT framework which identified the problem, objectives, alternatives, consequences, and tradeoffs to guide us toward a strategy for implementation of a set of actions for CRU communications.

Results of the SDM workshop included the development of a problem statement, an objectives hierarchy, a suite of alternatives that were evaluated using a consequences table and a clear process for assessing tradeoffs among alternative communication actions and strategies. Through the evaluation of consequences of each action or campaign, the team developed both the assessment tool (for the future) and an immediate plan for communication product development and distribution. The consequences table for this problem was meant to be flexible to accommodate changes in CRU thematic priorities and can be easily updated with new objectives, measures, and alternatives. In addition, the weight placed on objectives may change as the Team moves forward; the ranking and scoring system used in the workshop can be easily updated. 

Overall, the working group identified three different actions or campaigns—Fact Sheets, Who Are We Campaign, and Alumni Campaign—that scored high in the prototype decision framework. However, the tradeoffs analysis indicated that each action(s) performed better on some objectives than others. The working group identified a need to therefore develop an implementation plan that is composed of individual actions that each target different objectives to potentially create a holistic and feasible communications strategy that performs well for all objectives. In addition, the SDM prototype developed a scalable, objective-based framework for effectively communication of the value and accomplishments of the CRU program.</description>
			<pubDate>Thu, 30 Apr 2026 13:39:25</pubDate>
			<category>Preprints.org</category>
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			<title>GT-Seq panel development for species identification and parentage analysis of closely related hybridising &lt;i&gt;Scaphirhynchus&lt;/i&gt; sturgeons</title>
			<author>Huang, Junman; Flamio Jr., Richard; Campbell, Nathan; DeLonay, Aaron; Buhman, Amy; Heist, Edward</author>
			<link>https://pubs.usgs.gov/publication/70274589</link>
			<description>&lt;p&gt;&lt;span&gt;Hatchery supplementation is vital for conserving dwindling fish populations. Effective augmentation requires distinguishing hatchery-origin from wild individuals and accurately identifying species, particularly in systems where closely related species coexist. Genetic monitoring is key to quantifying genetic differences, but conventional markers do not distinguish hybrids, especially backcrosses. Misidentifying hybrids in hatchery programs compromises wild gene pools because hatchery broodstock contributes to numerous offspring being released into the wild. Here, we present a workflow for developing and evaluating the Genotyping-in-Thousands by sequencing (GT-seq) single nucleotide polymorphism (SNP) panel for North American river sturgeons (&lt;/span&gt;&lt;i&gt;Scaphirhynchus&lt;/i&gt;&lt;span&gt;&amp;nbsp;spp.). This panel is designed to detect complex hybrid classes and to determine parent-offspring relationships. Our species identification panel (S-loci) contains 155 SNPs selected for high genetic differentiation (F&lt;/span&gt;&lt;sub&gt;ST&lt;/sub&gt;&lt;span&gt;) between Pallid Sturgeon (&lt;/span&gt;&lt;i&gt;S. albus&lt;/i&gt;&lt;span&gt;) and Shovelnose Sturgeon (&lt;/span&gt;&lt;i&gt;S. platorynchus&lt;/i&gt;&lt;span&gt;), and the parentage assignment panel (P-loci) includes 112 SNPs with high heterozygosity within Pallid Sturgeon. Simulation analyses demonstrated that our GT-seq S-loci panel reliably classifies pure species, F1, F2 and backcross hybrids, even with up to 70% missing data. The P-loci panel achieves high-confidence parentage assignment with ≥ 80% typed loci, with performance influenced by the proportion of sampled parents. Overall, the novel&amp;nbsp;&lt;/span&gt;&lt;i&gt;Scaphirhynchus&lt;/i&gt;&lt;span&gt;&amp;nbsp;GT-seq panel developed in this study represents a robust and efficient tool for detecting hybridisation, assigning parentage and providing critical information for management decisions in ongoing Pallid Sturgeon conservation.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Wed, 1 Apr 2026 16:19:38</pubDate>
			<category>Molecular Ecology Resources</category>
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			<title>Peak-, mean-, and low-streamflow regional-regression equations for natural streamflow in central and western Colorado, 2019</title>
			<author>Kohn, Michael; Mast, M.; Gross, Tara</author>
			<link>https://pubs.usgs.gov/publication/sir20255047</link>
			<description>&lt;p&gt;The U.S. Geological Survey (USGS), in cooperation with the Colorado Department of Transportation, developed peak-, mean-, and low-streamflow regional-regression equations for estimating various statistics for natural streamflow in hydrologic regions of central and western Colorado. The peak-streamflow regression equations were developed using data from 418 streamgages, consisting of 15,202 years of record and a mean of approximately 36 years of record per streamgage. The mean- and low-streamflow regional-regression equations were developed using data from 323 streamgages where daily streamflow data were collected year-round. The annual exceedance-probability discharges for each streamgage were computed using the USGS software program PeakFQ. Mean monthly and 7-day minimum and maximum streamflows were computed using the USGS software program SWToolbox. Streamflow-duration values were computed using an R script. The regional-regression equations were determined using data for the period of record for a given streamgage through water year 2019. Geographic information systems datasets were used to develop 55 basin and 42 climatic characteristics, which were evaluated as candidate explanatory variables in the regression analysis.&lt;/p&gt;&lt;p&gt;For the peak-streamflow regional-regression equations, the study area was divided into four hydrologic regions based on mean basin elevation, including the Plateau (less than 8,014 feet), Mid-Elevation (8,015 feet to 9,492 feet), Sub-Alpine (9,493 feet to 10,490 feet), and Alpine (greater than 10,490 feet) regions. For the peak-streamflow equations, the selection of basin and climatic characteristics was based on the 1-percent annual exceedance-probability discharge for each hydrologic region.&lt;/p&gt;&lt;p&gt;For the mean streamflow, streamflow-duration values, and 7-day minimum and maximum streamflows, the study area was divided into four hydrologic regions based on river basin, including the (1) Colorado-East Slope Headwaters, (2) Green River, (3) Rio Grande, and (4) San Juan-Dolores. For mean streamflows, basin and climatic characteristics were evaluated separately for the annual period and each month for each hydrologic region. Regional regression equations published in this report are available for use in the USGS web-based program StreamStats.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 14:02:35</pubDate>
			<category>Scientific Investigations Report</category>
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			<title>Cumulative effects of multiple stressors on marine mammals: Elephant seals as a model system</title>
			<author>Costa, Daniel; Holser, Rachel; Shipway, Garrett; Favilla, Arina; McDonald, Birgitte; Shen, Daphne; Diluzio, Amber; Peterson, Sarah; Ackerman, Joshua; Crocker, Daniel</author>
			<link>https://pubs.usgs.gov/publication/70275309</link>
			<description>&lt;p&gt;&lt;span&gt;Noise exposure is a potential stressor for free-ranging marine mammals and is often studied in the absence of other environmental factors. Here, a multi-investigator, interdisciplinary effort was undertaken to examine the response of elephant seals to multiple stressors. An integrated physiological and ecological approach was taken, including immunology, stress physiology, toxicology, animal behavior, population biology, and life history theory, to examine the cumulative effects of exposure to multiple stressors in elephant seals. While we measured the response of individual animals, a population response can be predicted by incorporating these results into the long-term data on elephant seal demographics.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Tue, 28 Apr 2026 16:12:10</pubDate>
			<category></category>
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			<title>Uranium—Deposits, production and resources, market dynamics, and supply chain risks</title>
			<author>Mihalasky, Mark</author>
			<link>https://pubs.usgs.gov/publication/fs20253057</link>
			<description>&lt;h1&gt;Introduction&lt;/h1&gt;&lt;p&gt;&lt;span data-olk-copy-source=&quot;MessageBody&quot;&gt;Interest in nuclear power for the generation of electricity has risen with the increase in the need for more diverse baseload power, enhanced energy security, and the development of new technologies, such as small modular reactors (SMRs), which could provide power for remote areas, industrial applications, and artificial intelligence (AI) data centers. In 2024, the U.S. Department of Energy received $2.7 billion in congressional funding to bolster the domestic uranium production and nuclear fuel supply chain and address reliance on imports from foreign suppliers. In 2025, the U.S. Government issued several Executive and Secretary’s orders aimed at revitalizing the U.S. nuclear sector. If SMRs are to be as widely deployed in the United States and worldwide as envisioned, demand for uranium (nuclear reactor fuel) will likely increase.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span data-olk-copy-source=&quot;MessageBody&quot;&gt;After the Fukushima nuclear accident in 2011, the market spot price of uranium began a decline, followed by a decrease in U.S. and global uranium exploration and mine development expenditures that led to a uranium supply deficit until 2020, when prices started to recover, prompting a resurgence in uranium exploration and development. In January of 2024, the uranium spot price rose to a 17-year high $106 (U.S. dollars) per pound of U3O8 (triuranium oxide, commonly known as “yellowcake”), which is expected to increase uranium exploration, mine development, and uranium production domestically and worldwide.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 24 Apr 2026 18:39:05</pubDate>
			<category>Fact Sheet</category>
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			<title>Metallurgical coal—Deposits, production, resources, market dynamics, and supply chain risks</title>
			<author>Shaffer, Brian N.; Alonso, Elisa; Johnston, Michelle; Kinney, Scott</author>
			<link>https://pubs.usgs.gov/publication/fs20263061</link>
			<description>&lt;h1&gt;Plain Language Summary&lt;/h1&gt;&lt;p&gt;Metallurgical coal (met coal; consumed to produce coke for steelmaking) must meet specific chemical and physical specifications. In 2023, the conterminous United States produced 66 million short tons (mst) of met coal, consumed 15.85 mst domestically, exported 51.1 mst, and imported 0.7 mst. Most met coal was produced in the Appalachian Basin, but there are also resources that meet the specifications for met coal in the Western United States.&lt;/p&gt;</description>
			<pubDate>Fri, 24 Apr 2026 18:49:52</pubDate>
			<category>Fact Sheet</category>
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			<title>Cyanobacterial bloom occurrence and emergency department visits for asthma or wheeze, Wisconsin, 2017–2019</title>
			<author>Lavery, Amy; Murray, Jordan; Pennington, Audrey; Schaeffer, Blake; Seegers, Bridget; Hilborn, Elizabeth; Loftin, Keith; Scroggins, Stephen; Backer, Lorraine</author>
			<link>https://pubs.usgs.gov/publication/70275268</link>
			<description>&lt;h3&gt;Background:&amp;nbsp;&lt;/h3&gt;&lt;p&gt;Cyanobacterial harmful algal blooms (cyanoHABs) pose risks to human and animal health.&lt;/p&gt;&lt;h3&gt;Methods:&amp;nbsp;&lt;/h3&gt;&lt;p&gt;We investigated the relationship between cyanoHABs and asthma or wheeze-related emergency department (ED) visits near three Wisconsin cities (Green Bay, Madison, and Oshkosh) during 2017–2019. CyanoHAB exposure was approximated using the Cyanobacterial Assessment Network remotely sensed satellite indicator of cyanobacterial biomass, a chlorophyl algorithm (Chl&lt;sub&gt;BS&lt;/sub&gt;) aggregated by water-adjacent ZIP Code Tabulation Areas (ZCTA), and distance weighted from the nearest waterbody. Weekly counts of ED visits for asthma or wheeze were aggregated by ZCTA. Poisson generalized linear models estimated the association between the weekly number of ED visits and weekly Chl&lt;sub&gt;BS,&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;adjusting for maximum temperature, dewpoint, fine particulate matter (PM&lt;sub&gt;2.5&lt;/sub&gt;), month, and correlation within ZCTA.&lt;/p&gt;&lt;h3&gt;Results:&amp;nbsp;&lt;/h3&gt;&lt;p&gt;During 2017–2019, 7,057 ED visits for asthma or wheeze occurred in the study area (42 ZCTAs). Peaks in Chl&lt;sub&gt;BS&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;occurred between June and October, with higher values in Lake Winnebago and Lake Mendota compared to Green Bay. Chl&lt;sub&gt;BS&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;was not associated with ED visits for asthma or wheeze (adjusted rate ratio = 1.00, 95% confidence interval = 0.99, 1.00), and the presence of onshore winds did not change this result. Monthly aggregations of ED visits and Chl&lt;sub&gt;BS&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;showed a monotonic trend between increasing Chl&lt;sub&gt;BS&lt;/sub&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;and ED visits during July–September.&lt;/p&gt;&lt;h3&gt;Conclusion:&amp;nbsp;&lt;/h3&gt;&lt;p&gt;This study demonstrates the utility of remote sensing data in environmental health research. Future studies could explore individual-level exposure and outcomes to refine health risks associated with cyanoHABs.&lt;/p&gt;</description>
			<pubDate>Thu, 7 May 2026 15:56:42</pubDate>
			<category>Environmental Epidemiology</category>
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			<title>Development of a two-stage lifecycle model to inform the trap-and-haul program for &lt;em&gt;Oncorhynchus kisutch&lt;/em&gt; (coho salmon) in the Lewis River, Washington</title>
			<author>Plumb, John; Perry, Russell</author>
			<link>https://pubs.usgs.gov/publication/ofr20261004</link>
			<description>&lt;p&gt;Restoration of salmon populations in the upper Lewis River Basin, Washington, depends on a trap-and-haul program owing to the Lewis River Hydroelectric Project (hereinafter referred to as “Project”) operated by PacifiCorp and Cowlitz Public Utilities District (hereinafter referred to as “Utilities”), which has been a barrier to salmon passage since the 1930s. Thus, sustaining the &lt;i&gt;Oncorhynchus kisutch&lt;/i&gt; (Walbaum, 1792; coho salmon) population upstream from the Project currently depends on two fundamental factors: (1) the collection of upstream migrating adult coho salmon at Merwin Dam, the lowermost dam within the Project, and transporting them by truck to spawn above Swift Dam, the uppermost dam within the Project; and (2) the collection of out-migrating juvenile coho salmon at the downstream collection facility at Swift Dam for transport and release below the Project. The reintroduction program began once the downstream collection facility at Swift Dam was commissioned in late 2012, with the first year of transport data being collected in 2013. Over the past decade, the Utilities have been collecting data on juvenile outmigrants and adult fish returns at the dams. The need to construct a lifecycle model for Lewis River anadromous fish was identified by the Lewis River Aquatic Technical Subgroup, with the understanding that many years (more than 15 years) of data collection are needed to adequately measure the lifecycle production of salmon. The U.S. Geological Survey was contracted to develop and apply the model to past data at the Lewis River dams to help inform future data collection and provide a framework that can be updated annually to measure trap-and-haul program performance within a lifecycle context.&lt;/p&gt;&lt;p&gt;Because coho salmon can live as long as 5 years, estimating demographic parameters for coho salmon populations over their lifecycle requires at least 10 or more years of data collection. Over the past decade, PacifiCorp has been collecting data on fish collection efficiency and the numbers of adult and juvenile salmon transported around the Lewis River dams, making this an ideal time to formulate a lifecycle model that can guide future data collection efforts and provide preliminary information to resource managers. The goal of the statistical lifecycle model is to estimate annual production and survival during two critical life-stage transitions: (1) the freshwater production from escapement of adults released upstream from Swift Dam, and the collection of downstream migrating juveniles at the downstream passage facility at Swift Dam; and (2) the smolt-to-adult survival from the time of collection at Swift Dam to their return as adults. We used the Beverton-Holt stock-recruitment model to estimate juvenile production from the number of spawners (Beverton and Holt, 1957). This approach allowed us to test for density dependence at current spawner abundances while estimating annual productivity, defined as the number of juveniles produced per spawner at low spawner abundance. Productivity was then expressed as a function of the number of juveniles collected and transported downstream from the Project. Because juvenile fish collection efficiency (FCE) directly affects the number of juveniles that survive to continue downstream migration, FCE is a primary determinant of fish production. Consequently, the modeling framework is well suited to evaluate the performance of trap-and-haul programs within a lifecycle context.&lt;/p&gt;&lt;p&gt;The objectives of this study were to (1) gather and collate available data on adult and juvenile coho salmon at Merwin and Swift Dams; (2) quantify adult escapement, juvenile abundance, and the age at outmigration and adult return; (3) describe, formulate and fit the integrated population model to the data; and (4) summarize our findings, identify data gaps, and identify opportunities for future studies that could improve model estimation and inference. Our key findings were: (1) over and above the number of spawning females, FCE was the primary factor affecting productivity of coho salmon above Swift Dam; (2) smolt-to-adult return (SAR) rates were relatively high considering that harvest was included in the estimate, averaging about 4.5 percent and ranging as high as 12.9 percent; and (3) juvenile capacity upstream from Swift Dam was difficult to estimate due to the limited range in spawning females over the time series of data, suggesting the model may be improved by collecting data at higher spawner abundances. In addition, by including FCE in the model, we estimated that the median pre-collection productivity, defined as the number of juveniles produced per spawner when FCE=1, was 64 juveniles per spawner. Because the two-stage lifecycle model partitions factors that affect fish production in rivers versus the ocean, the model estimates may help inform fishery managers about the overall role that fish collection at Swift Dam plays in the recovery and sustainability of Lewis River coho salmon. By providing the model with (1) more years of data, (2) higher numbers of spawning females, and (3) data on age at juvenile migration in relation to age at adult return, greater certainty in the estimates of capacity and SAR can be attained. Ultimately, information provided by the model may assist in the evaluation and continued improvement of the current trap-and-haul program to support anadromous fishes in the Lewis River Basin.&lt;/p&gt;</description>
			<pubDate>Thu, 23 Apr 2026 13:56:24</pubDate>
			<category>Open-File Report</category>
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			<title>Assessment of undiscovered shale-gas resources in the Grand Erg/Ahnet Basin Province of Algeria, 2026</title>
			<author>Brownfield, Michael; Schenk, Christopher; Mercier, Tracey; Tennyson, Marilyn E.; Woodall, Cheryl; Finn, Thomas; Le, Phuong A.; Leathers-Miller, Heidi M.; Pitman, Janet K.; Drake, Ronald M.; Gaswirth, Stephanie</author>
			<link>https://pubs.usgs.gov/publication/fs20263005</link>
			<description>&lt;p class=&quot;MsoNormal&quot;&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;Using a geology-based assessment methodology, the U.S. Geological Survey estimated undiscovered, technically recoverable mean resources of 80.1 trillion cubic feet of shale gas in the Grand Erg/Ahnet Basin Province of Algeria.&lt;/p&gt;</description>
			<pubDate>Wed, 22 Apr 2026 20:02:30</pubDate>
			<category>Fact Sheet</category>
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			<title>Fish body midline segmentation using binary search</title>
			<author>Sterling, Robert; Goerig, Elsa; Buzdalov, M; Castro-Santos, Theodore; Akanyeti, O.</author>
			<link>https://pubs.usgs.gov/publication/70275215</link>
			<description>&lt;p&gt;&lt;span&gt;Body and caudal fin locomotion is ubiquitous in aquatic vertebrates, and kinematic models describing it are used in robotics, biomechanics and fisheries research. This paper presents a new algorithm to translate continuous body midlines of fish into a series of interconnected segments by identifying favorable joint positions along the body. The algorithm employs binary search to generate parsimonious kinematic models, aiming at minimizing the number of segments yet keeping approximation error below a user-defined threshold. To achieve this, the algorithm maximizes the length of each segment by determining the most distal joint position through repetitive shrinking of the search space. Theoretical and empirical analysis using two different datasets show that the binary search algorithm is substantially faster when compared to segment growing algorithm, which employs linear search to generate its models. There is four-fold improvement in computation time when generating models with less than 10 segments, which are typically sufficient to describe fish and fish-inspired robot movements. Furthermore, the multi-segment models generated by the binary search algorithm matched the ground truth models obtained through dynamic programming in over 97% of cases, and on average, contained one fewer segment than those produced by the Ramer–Douglas–Peucker algorithm, which is widely used in curvature simplification tasks. Our findings suggest that the binary search algorithm provides a computationally efficient approach for generating compact kinematic models and may facilitate the analysis of large datasets with high temporal and spatial resolution.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 23 Apr 2026 15:07:26</pubDate>
			<category>Computers and Electronics in Agriculture</category>
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			<title>Spatially consistent but temporally divergent changes in nitrate and phosphorus loads and yields in Illinois watersheds, 1997–2022</title>
			<author>Kamrath, Brock; Murphy, Jennifer; Schafer, Lindsey; Podzorski, Hannah; McIsaac, Gregory</author>
			<link>https://pubs.usgs.gov/publication/70275332</link>
			<description>&lt;p&gt;&lt;span&gt;Illinois contributes substantial nutrient loads to the Gulf of America, warranting watershed-scale assessment. This study estimated nitrate-nitrogen (nitrate-N) and total phosphorus (TP) loads and yields for 49 Illinois 8-digit hydrologic unit code (HUC8) watersheds draining to the Mississippi River Basin from 1997–2022, comparing recent (2018–2022) to baseline (1997–2011) conditions. Estimates included point and nonpoint source contributions, dissolved phosphorus, and water yields. During the recent period, nonpoint sources dominated nutrient export (82% nitrate-N, 78% TP), though point sources drove high yields in the Chicago area. Spatially, nonpoint source nutrient hotspots persisted with nitrate-N yields highest in east-central and northern Illinois and TP yields higher in southern and western Illinois. Temporally, statewide nitrate-N loads decreased 9%, while TP loads increased 27%. Nitrate-N yields increased in 22 HUC8s and decreased in 20, while TP yields increased in 32 HUC8s and decreased in 9. For both nutrients, baseline yields were negatively correlated with yield changes, indicating high-yielding watersheds tended toward larger decreases or smaller increases. Water yields increased 19% on average but were weakly correlated with nutrient yield changes (&lt;/span&gt;&lt;i&gt;r&lt;/i&gt;&lt;span&gt; = 0.23 and 0.20 for nitrate-N and TP). These results reveal spatially persistent yet temporally divergent nutrient export across Illinois, with contrasting nitrate-N and TP trajectories for nonpoint sources.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Wed, 29 Apr 2026 15:01:54</pubDate>
			<category>Journal of American Water Resources Association</category>
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			<title>Spatial heterogeneity of salt marsh vulnerability to sea-level rise: Dual controls of hydrological setting and salinity regime</title>
			<author>Yin, Dongxiao; Defne, Zafer; Ganju, Neil K.; Warner, John C.; Ralston, David; Harris, Courtney; Li, Bin</author>
			<link>https://pubs.usgs.gov/publication/70275228</link>
			<description>&lt;p&gt;&lt;span&gt;Salt marsh vulnerability to sea-level rise (SLR) is typically assessed using point measurements of vertical accretion, neglecting three-dimensionality of geomorphic evolution and spatial variability. Recent studies suggest links between vertical and horizontal vulnerability, with differences between oligohaline and polyhaline marshes, yet these relationships remain untested in estuary-marsh systems. Here we combine geospatial analysis with hydrodynamic modeling to evaluate how unvegetated/vegetated marsh ratio (UVVR), a metric of marsh degradation, relates to elevation across hydrological regions and salinity regimes in the Albemarle-Pamlico Estuarine System, the largest lagoonal estuary in U.S. We show that at given normalized elevation, UVVR decreases across hydrological regions and salinity regimes from offshore to inland. UVVR-elevation relationship varies systematically with both hydrological setting and salinity regime, with hydrology exerting stronger influence. These findings challenge the assumption of a universal marsh deterioration trajectory and underscore the need to account for spatial heterogeneity when predicting responses to SLR.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 23 Apr 2026 14:59:21</pubDate>
			<category>Geophysical Research Letters</category>
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			<title>Dynamic drainage reorganization in Eastern Tibet: Insights from the Yangtze River first bend</title>
			<author>Zhao, Xudong; Li, Yifei; Zhang, Huiping; Lease, Richard; Wang, Ying; Hao, Yuqi; Ma, Zifa; Xie, Hao; Kang, Huan; Xiong, Jianguo; Zhang, Peizhen</author>
			<link>https://pubs.usgs.gov/publication/70275367</link>
			<description>&lt;p&gt;&lt;span&gt;The modern drainage network of eastern Tibet is widely believed to have developed through a series of river capture and flow reversal events; however, the timing and mechanisms driving this reorganization remain contentious. Among these events, the river capture that formed the First Bend of the Yangtze River (YFB) stands out as both iconic and particularly debated. Here we present sedimentary provenance data from the Late Miocene–Quaternary Dali Basin, located south of the YFB, which indicate that a southward-flowing Jinsha River (i.e., the present-day upper Yangtze River) sourced sediment to the Dali basin at ∼7.4–6.4 Ma in a drainage configuration different from that of today. Because this interval postdates the initial establishment of a near-modern Jinsha River system prior to the Miocene, our results imply at least two discrete fluvial reorganizations occurred at the YFB—one preceding ∼7.4 Ma and another following ∼6.4 Ma. By integrating these findings with landscape evolution modeling, we infer that the initiation of rapid uplift of the Yulong-Haba Mountains and the Diancang Shan may have been responsible for these drainage reorganizations. These results underscore that Cenozoic drainage systems on the eastern Tibetan Plateau have evolved dynamically on a short timescale of ∼10&lt;/span&gt;&lt;sup&gt;5&lt;/sup&gt;&lt;span&gt;–10&lt;/span&gt;&lt;sup&gt;6&lt;/sup&gt;&lt;span&gt;-year, rather than remaining in a long-term stationary configuration on ∼10&lt;/span&gt;&lt;sup&gt;7&lt;/sup&gt;&lt;span&gt;-year timescales.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 1 May 2026 15:26:27</pubDate>
			<category>Earth and Planetary Science Letters</category>
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			<title>Geophysical architecture and geochronology of the Neoarchean Mentor anorthosite intrusive complex, northwestern Minnesota: Largest anorthosite complex of the Superior Province?</title>
			<author>Drenth, Benjamin; Radakovich, Amy; Souders, Amanda Kate; Hudak, George; Saari, Stacy</author>
			<link>https://pubs.usgs.gov/publication/70275286</link>
			<description>&lt;p&gt;&lt;span id=&quot;_mce_caret&quot; data-mce-bogus=&quot;1&quot; data-mce-type=&quot;format-caret&quot;&gt;&lt;span&gt;The Neoarchean Mentor anorthosite intrusive complex (MAIC) lies within the Wawa subprovince in northwestern Minnesota, in a region where the Wawa, Quetico, and Wabigoon subprovinces are juxtaposed in close proximity. Archean rocks are entirely concealed, and interpretations are developed from aeromagnetic, gravity, and borehole samples. The MAIC includes both anorthosite (dense, weakly magnetized) and oxide-rich gabbro (strongly magnetized) lithologies. Anorthosite is coarse-grained to megacrystic, intensely altered, and locally brecciated. Pervasive epidote alteration enhanced the density of the anorthosite via introduction of higher-density mineral assemblages, explaining why the MAIC produces a significant gravity high. Oxide-rich gabbro forms a border phase of the MAIC and has potential for vanadium, chromium, and titanium mineralization, and produces a strong aeromagnetic high. The MAIC is interpreted to extend over an area of 640&amp;nbsp;km&lt;/span&gt;&lt;sup&gt;2&lt;/sup&gt;&lt;span&gt;, making it the largest known anorthosite complex of the Superior Province, as measured by preserved areal extent. Modeling indicates the MAIC extends more than 6&amp;nbsp;km into the subsurface. A new Pb–Pb zircon age of 2737.2&amp;nbsp;±&amp;nbsp;4.5 Ma is interpretated as the crystallization age of anorthosite within the MAIC, showing that the MAIC formed well before the ca. 2690 Ma Shebandowanian orogeny, and raising new questions about correlations with other parts of the Wawa subprovince. A low-density batholith, here informally called the Fertile batholith, is interpreted to intrude the southern part of the MAIC. A new Pb–Pb zircon age of 2701.1&amp;nbsp;±&amp;nbsp;6 Ma is interpreted as the magmatic age of the Fertile batholith.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 27 Apr 2026 15:02:08</pubDate>
			<category>Canadian Journal of Earth Sciences</category>
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			<title>A site prioritization tool for invasive species management: Integrating diverse spatial data to improve decision making</title>
			<author>Prevéy, Janet; Reimer, Cameron; Engelstad, Peder; Belamaric, Pairsa; Hogan, Terri; LaRoe, Jillian; Mumford, Colter; Sieracki, Jennifer; Jarnevich, Catherine</author>
			<link>https://pubs.usgs.gov/publication/70275607</link>
			<description>&lt;p&gt;&lt;span id=&quot;_mce_caret&quot; data-mce-bogus=&quot;1&quot; data-mce-type=&quot;format-caret&quot;&gt;&lt;span&gt;Resource managers are tasked with protecting natural areas from invasive species with limited resources. Further, invasive management goals can vary greatly based on different management priorities specific to management agencies or taxa of interest. The site prioritization tool for invasive species management addresses these challenges by creating a platform to view and combine diverse spatial data layers to estimate cumulative invasion risk based on user-specific needs. For this tool, we developed a human transport risk layer, estimating invasion risk based on proximity to human population centers and transportation corridors, and created maps of non-native species richness across the conterminous United States. The tool also includes spatial layers showing projected changes in key climate variables through the end of the century to identify areas where invasion risk may shift. Users can explore these layers to prioritize sites based on the invasive taxa of interest, likely invasion pathways, and disturbances that may elevate invasion risk. This interactive tool will allow managers to make the spatial comparisons needed to focus efforts on areas that are highly susceptible to invasion and efficiently target monitoring and suppression efforts.&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Tue, 5 May 2026 14:55:27</pubDate>
			<category>Ecological Informatics</category>
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			<title>Non-native invasive beetle alters structure of a riparian bird community in a biodiversity hotspot</title>
			<author>Kus, Barbara E.; Yee, Julie; Mendia, Shannon M.</author>
			<link>https://pubs.usgs.gov/publication/70275358</link>
			<description>&lt;p&gt;&lt;span&gt;A serious emerging threat to southern California riparian ecosystems is the invasive shot hole borer (&lt;/span&gt;&lt;i&gt;Euwallacea&lt;/i&gt;&lt;span&gt;&amp;nbsp;spp.; SHB), a non-native beetle that cultivates a pathogenic fungus that kills trees of 66 reproductive host species. We examined the response of the bird community at the Tijuana River, California, to a massive SHB infestation in 2015 using data from a Monitoring Avian Productivity and Survivorship (MAPS) station operated during 7 pre-infestation (2009-15) and 7 post-infestation (2017-23) years. Species richness did not change between pre- and immediate (2017-18) post-SHB periods, but average annual adult captures declined by 27%. Among the species making up ≥ 5% of the total individuals caught in any one year (n=15), abundance declined by up to 76% in 10 species, including those most abundant at the station (Bushtit (&lt;/span&gt;&lt;i&gt;Psaltriparus minimus&lt;/i&gt;&lt;span&gt;), Song Sparrow (&lt;/span&gt;&lt;i&gt;Melospiza melodia&lt;/i&gt;&lt;span&gt;), Common Yellowthroat (&lt;/span&gt;&lt;i&gt;Geothlypis trichas&lt;/i&gt;&lt;span&gt;), Orange-crowned Warbler (&lt;/span&gt;&lt;i&gt;Leiothlypis celata&lt;/i&gt;&lt;span&gt;), and Wilson’s Warbler (&lt;/span&gt;&lt;i&gt;Cardellina pusilla&lt;/i&gt;&lt;span&gt;)). Mean annual abundance increased slightly for the endangered Least Bell’s Vireo (&lt;/span&gt;&lt;i&gt;Vireo bellii pusillus&lt;/i&gt;&lt;span&gt;) and Northern Yellow Warbler (&lt;/span&gt;&lt;i&gt;Setophaga aestiva&lt;/i&gt;&lt;span&gt;) and doubled for House Finch (&lt;/span&gt;&lt;i&gt;Haemorhous mexicanus&lt;/i&gt;&lt;span&gt;) and Western Warbling-Vireo (&lt;/span&gt;&lt;i&gt;V. swainsoni&lt;/i&gt;&lt;span&gt;). We compared species trends at the Tijuana River to those at a nearby uninfested MAPS station on the Santa Margarita River to isolate the effect of SHB from other factors influencing annual abundance. The contribution of SHB to changes in abundance post-SHB was high (63-80%) for 7 declining species, moderate (22-45%) for 4 species, and weakly to moderately positive (18-40%) for 3 species. By 2019, the SHB infestation at the Tijuana River had abated and canopy cover was recovering through resprouting of mature willows (&lt;/span&gt;&lt;i&gt;Salix&lt;/i&gt;&lt;span&gt;&amp;nbsp;spp.) and seedling establishment. Bird abundance tracked this regrowth, with all of the species strongly affected by SHB increasing between 2019-23. The rapid recovery of the Tijuana River habitat and the associated response by the bird community are encouraging signs that the threat of the invasive shot hole borer to regional biodiversity may not be as great as originally anticipated.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 30 Apr 2026 15:17:01</pubDate>
			<category>Frontiers in Ecology and Evolution</category>
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			<title>Surface rupture and slip distribution of the 2025 Mw7.7 Mandalay earthquake and updated length scaling of supershear earthquakes</title>
			<author>Reitman, Nadine; Wang, Yuanshi; Kuo, Yu-Ting; Hanagan, Catherine Elise; Hatem, Alexandra; DuRoss, Christopher; Chen, Chun-Chi; Goldberg, Dara; Yin, Harriet; Briggs, Richard; Thompson Jobe, Jessica; Nicovich, Sylvia; Lynch, Emerson; Powell, Joseph; Barnhart, William; Schmitt, Robert</author>
			<link>https://pubs.usgs.gov/publication/70275602</link>
			<description>&lt;p&gt;The 2025 &lt;strong&gt;&lt;i&gt;M&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt;&lt;/strong&gt; 7.7 Mandalay, Burma (Myanmar), earthquake ruptured 475 km of the central Sagaing fault and is the longest continental strike-slip rupture on record. The observed rupture length is 1.6–4.7 times the value expected (100–300 km) from existing length-magnitude scaling relations for strike-slip earthquakes. The earthquake resulted from shallow dextral faulting and ruptured bilaterally with supershear speeds south of the epicenter, rupturing close to three major cities in Myanmar and exposing over six million people to violent or extreme shaking. We report on the surface rupture character, length, and slip distribution based on sub-pixel correlation of Sentinel-2 (10 m) and Planet Dove (3 m) optical images and visual analysis of SkySat and WorldView (0.3–0.5 m) optical images. The earthquake had moderate surface slip (average = 3.3 m, maximum = 5.6 m, 25–75% range = 3.0–4.0 m), narrow deformation zone width (1–10 pixels in sub-pixel correlation and up to 190 meters for the detailed surface rupture mapping), and simple fault geometry (no stepovers or large changes in strike, 87% of the rupture that was mapped in detail is single-stranded). We attribute the extreme length of the Mandalay earthquake to supershear rupture speed, simple fault geometry, narrow down-dip width, and moderate surface slip. Based on a compilation of 25 supershear strike-slip earthquakes (&lt;i&gt;&lt;strong&gt;M&lt;/strong&gt;&lt;/i&gt;&lt;strong&gt;&lt;sub&gt;w&lt;/sub&gt;&lt;/strong&gt;&amp;nbsp;6.5–8.6; 1979–2025), we find that the rupture length of supershear earthquakes does not fit empirical scaling relationships for strike-slip earthquakes that predict length from magnitude. A length-magnitude scaling relationship based on supershear earthquakes has a best fit of &lt;strong&gt;log&lt;sub&gt;10&lt;/sub&gt;&lt;/strong&gt;(surface rupture length) = 0.89 &lt;strong&gt;&lt;i&gt;M&lt;/i&gt;&lt;sub&gt;w&lt;/sub&gt; &lt;/strong&gt;– 4.44, indicating that supershear earthquakes tend to be longer than their subshear counterparts for any given magnitude and thus may expose a greater population to shaking.&lt;/p&gt;</description>
			<pubDate>Tue, 5 May 2026 16:39:48</pubDate>
			<category>Seismological Research Letters</category>
		</item>
		<item>
			<title>Standardized method for logging drill core at the Idaho National Laboratory, Idaho</title>
			<author>Dietz, Haley</author>
			<link>https://pubs.usgs.gov/publication/tm5E1</link>
			<description>The U.S. Geological Survey’s (USGS) Lithologic Core Storage Library (CSL) at the Idaho National Laboratory stores more than 120,000 feet of drill core that is accessible to the public for research and sampling. To effectively convey the physical and descriptive properties of the drill core, USGS staff at the Idaho National Laboratory Project Office log the drill core and publish the lithologic logs as data releases. The logs provide essential data on the lithology, texture, mineralogy, alteration, and other physical properties of the core, which serve as valuable information for researchers to guide their research and sampling efforts. To ensure consistent, quality, and dependable lithologic logs, this document outlines the procedures and expectations for logging drill core at the CSL. This document describes the processes for storing, photographing, and logging core, and includes a variety of resources, reference materials, and appendixes designed to standardize and aid the logging process. Following the procedures outlined in this document will produce consistent, detailed logs that facilitate dependable observations and serve as an easy reference for researchers and other interested parties.</description>
			<pubDate>Tue, 21 Apr 2026 14:52:03</pubDate>
			<category>Techniques and Methods</category>
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		<item>
			<title>Assessment of groundwater quantity and quality contributions to Lake Huron</title>
			<author>Kaemming, Bridget; Ford, Chanse; Martin, Sherry</author>
			<link>https://pubs.usgs.gov/publication/sir20265136</link>
			<description>&lt;p&gt;Lake Huron, one of the five Great Lakes, borders the United States and Canada, with Michigan as the only U.S. State on its shoreline. Like other freshwater lakes, it faces water-quality challenges from nutrients and chemicals applied across its drainage basin. Although past studies focused on surface-water sources, groundwater contributions remain less understood. To address this gap, the U.S. Geological Survey, as part of the Cooperative Science and Monitoring Initiative, classified drainage basins to Lake Huron into eight hydrogeologic zones based on bedrock rock type and glacial sediment transmissivity. Utilizing existing data and empirical field data, we quantified groundwater discharge and identified areas of concern for loading of chloride and nitrate to Lake Huron. Groundwater contributions, including indirect and shoreline discharge, ranged from 5.8 to 11.5 inches annually, totaling 1.9 cubic miles and 0.09 cubic mile, respectively. Hydrogeologic zones with higher glacial sediment transmissivity yielded greater indirect groundwater discharge. Chloride levels above the U.S. Environmental Protection Agency’s 250-mg/L recommendation were mainly in the Saginaw lowlands, whereas nitrate above the 10-mg/L standard was rare—found in only 11 wells. Together, the analysis of where groundwater discharge is occurring in the Lake Huron Basin and the identification of areas with potential groundwater-quality concerns can help prioritize areas that are critical to protecting the long-term health of Lake Huron.&lt;/p&gt;</description>
			<pubDate>Fri, 24 Apr 2026 18:36:33</pubDate>
			<category>Scientific Investigations Report</category>
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		<item>
			<title>Annotated bibliography of scientific research on new world screwworm (&lt;i&gt;Cochliomyia hominivorax&lt;/i&gt;) myiasis in wildlife</title>
			<author>Timbie, Sarah; Weidenkopf, Shelby Jo; Grear, Daniel</author>
			<link>https://pubs.usgs.gov/publication/ofr20261006</link>
			<description>&lt;p&gt;The New World screwworm (&lt;i&gt;Cochliomyia hominivorax&lt;/i&gt;; NWS) is a parasitic blowfly that lays its eggs in open wounds of live, warm-blooded animals including livestock, wildlife, and potentially humans. The larvae consume living animal tissue, and if untreated, the infestation can lead to death. Although NWS was eradicated in the United States in 1966, it has been moving northward from its endemic range in South America during the past decade and could seriously threaten the health of U.S. wildlife populations, making detection, treatment, and surveillance of the disease far more difficult across this multi-sector disease system.&lt;br&gt;As the likelihood of NWS reintroduction to the United States increases, veterinarians, wildlife managers, and conservation specialists need to be informed and prepared to respond. The existing knowledge about NWS interactions with wildlife hosts is lacking, especially regarding North American species where the NWS has been eradicated for more than 50 years. To address this knowledge gap, we compiled an annotated bibliography that consolidates key information from the existing literature on NWS infestation in wild animals.&lt;/p&gt;</description>
			<pubDate>Tue, 28 Apr 2026 16:24:42</pubDate>
			<category>Open-File Report</category>
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		<item>
			<title>A novel drive-point multilevel system to investigate PFAS and other contaminants of global concern in the hyporheic zone of a wastewater effluent dominated stream</title>
			<author>Meyer, J.; Mianecki, A.; Occhi, E.; Kolpin, Dana W.; LeFevre, G.</author>
			<link>https://pubs.usgs.gov/publication/70275320</link>
			<description>&lt;p&gt;&lt;span&gt;Contaminants found in treated wastewater discharged to streams, including pharmaceuticals and per- and polyfluoroalkyl substances (PFAS), are of global concern due to their deleterious effects on aquatic ecosystems and potential impacts to human health. Hyporheic zones have strong potential for contaminant attenuation. Assessing this potential requires collection of physical and biogeochemical data within the hyporheic zone. This study tested the applicability of a novel drive-point multilevel system (DP-MLS) for quantifying head profiles and characterizing contaminant concentrations in the hyporheic zone of a temperate region effluent dominated stream (EDS). DP-MLS, each with 4 ports, were installed in the stream bed at two sites, DS-1 and DS-2, 0.2 and 4.7 km downstream of the effluent outfall, respectively. Head profiles were measured and groundwater collected for analysis of pharmaceuticals and PFAS temporally over two years. The DP-MLS withstood rapid changes in stage, ice formation, and floating debris. Vertical hydraulic gradients (VHG) were generally upward but varied in magnitude indicating heterogeneity in hydraulic conductivity and variability in flow conditions. Upward VHG were also about 2X larger at DS-1 than at DS-2. Contaminant concentration profiles consistently showed penetration of pharmaceuticals and PFAS to 1 m below the bed at DS-2 while there was less penetration, lower groundwater concentrations, and more temporal variability in concentrations at DS-1. Integration of the physical and chemical data suggests weaker upwelling conditions at DS-2 are more easily reversed during periods of high stream stage, which could facilitate migration of wastewater contaminants into the bed. However, further studies incorporating other transport processes and reach scale dynamics are required to fully characterize these exchanges. Overall, this study demonstrates the efficacy of these novel DP-MLSs for characterization of the hyporheic zone and provides new insights into the occurrence, composition, and persistence of wastewater derived contaminants in the hyporheic zone of a well-studied EDS.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Wed, 29 Apr 2026 14:14:57</pubDate>
			<category>Hydrological Processes</category>
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			<title>Line transect distance sampling and genetic analyses reveal a small but genetically diverse coastal Gopher Tortoise (Gopherus polyphemus) population</title>
			<author>Lamont, Margaret; Gallardo-Alanis, Irlanda; Chordia, Diya; Palandri, Michael; Chiari, Ylenia</author>
			<link>https://pubs.usgs.gov/publication/70275739</link>
			<description>&lt;p&gt;Gopher Tortoises inhabit coastal systems, including barrier islands, across the southeastern U.S. &amp;nbsp;St. Vincent National Wildlife Refuge is an uninhabited barrier island located off the coast of northwestern Florida. &amp;nbsp;Although tortoises have been observed on the island, no information is available on the status of the population. &amp;nbsp;We conducted a line transect distance sampling survey to evaluate the Gopher Tortoise population on St. Vincent Island. &amp;nbsp;Additionally, we collected samples for genetic analyses from 11 individual tortoises captured opportunistically and via bucket traps on the island and 15 tortoises captured at nearby mainland sites. &amp;nbsp;Surveys covered approximately 43% of the sampling frame and resulted in 55 burrows, 28 of which were occupied. &amp;nbsp;The abundance estimate for the island was 52 tortoises (95% confidence interval [CI] = 27–100) and the density was relatively low at 0.071 tortoises/ha (95% CI = 0.037–0.136). &amp;nbsp;Genetic analyses of two mtDNA markers identified a new haplotype unique to St. Vincent Island and another three haplotypes previously found across the southeastern U.S. &amp;nbsp;The genetic composition of Gopher Tortoises on St. Vincent Island is representative of the entire southeastern U.S. but most closely aligns with tortoise populations east of the Apalachicola-Chattahoochee River system. &amp;nbsp;Although the tortoise population on this island is small, the extent of seemingly appropriate habitat on the island and the genetic diversity of the population suggests the potential for growth with added management intervention.&lt;/p&gt;</description>
			<pubDate>Fri, 15 May 2026 13:40:58</pubDate>
			<category>Herpetological Conservation and Biology</category>
		</item>
		<item>
			<title>Quantitative mineral resource assessment of lithium pegmatite deposits in the northern Appalachian orogen, USA</title>
			<author>Wintzer, Niki; Holm-Denoma, Christopher S.; Poletti, Jacob; McCaffrey, Dalton; Mordensky, Stanley; Tharalson, Erik Roger; Cronkite-Ratcliff, Collin</author>
			<link>https://pubs.usgs.gov/publication/70274714</link>
			<description>&lt;p&gt;&lt;span&gt;Lithium demand is projected to increase more than 48 times by 2040 due to electric vehicle production and other energy storage needs. Most lithium production is outside of the USA, thereby increasing supply chain vulnerability. The combined end use importance and heightened supply risk of lithium make this lightest metallic element a critical commodity to the USA. To mitigate this supply risk, the US Geological Survey is actively assessing lithium deposits in the USA. Herein, we detail an assessment for lithium-mineralized pegmatites in the US northern Appalachian Mountains. Permissive tracts were generated by cross-referencing tectonic and geologic maps and mineral occurrence data with mappable criteria derived from generalized and region-specific lithium pegmatite ore deposit models; tracts were then ranked as having high, medium, or low permissibility. Available geophysical and geochemical data were found to be of minimal utility for this deposit type at the scale of the assessment. The number of undiscovered deposits were estimated and integrated into probabilistic simulations, which included an expanded and updated global grade and tonnage model of pegmatite-hosted lithium ore. The estimated total amount of undiscovered resources for the northern Appalachian Orogen has a median value of 1,410,000 metric tons of Li&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O when considering moderate correlation across sub-regions. At a confidence level of 90%, a resource of at least 90,000 metric tons of Li&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O remains undiscovered, and at a 10% confidence level, a resource of as much as 7,380,000 metric tons Li&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O remains undiscovered. After applying an up-to-date economic filter to convert median contained lithium to recoverable material, a correlated total of 900,000 metric tons of Li&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O may be economically extractable, equating to enough Li&lt;/span&gt;&lt;sub&gt;2&lt;/sub&gt;&lt;span&gt;O to provide the current annual US lithium supply deficit (presently obtained through net imports) for 127&amp;nbsp;years at 2025 rates of apparent consumption. This period of provision will inevitably shorten with projected increasing consumption rates, emphasizing that further research could be completed to better delineate regions of high lithium resource potential and support exploration and domestic production.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Mon, 20 Apr 2026 15:29:50</pubDate>
			<category>Natural Resources Research</category>
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		<item>
			<title>The role of groundwater in contributing to surface water salinization in the Upper Colorado River Basin</title>
			<author>Miller, Matthew; Miller, Olivia; Longley, Patrick; Wise, Daniel; McDonnell, Morgan; Schmadel, Noah; Alder, Jay</author>
			<link>https://pubs.usgs.gov/publication/70275185</link>
			<description>Freshwater salinization impacts the availability of water for human use and ecosystem needs worldwide. It has been estimated that total dissolved solids (TDS) in the Colorado River Basin cause $350 million/year in damages and substantial resources are devoted to reducing TDS loading to streams. This study describes the development and application of coupled watershed models that enable TDS source tracking through the subsurface and across the landscape at a seasonal timestep for 35 years in the Upper Colorado River Basin.  Results indicate that, on average, 75% of TDS loading to streams originates as baseflow, and 50% of loading is lagged in delivery by longer than one season.  Snowmelt was identified as a dominant process controlling the transport of lagged TDS to streams.  This approach informs when and where TDS mitigation efforts may be effective in a watershed that serves as a critical water supply for the southwestern United States.</description>
			<pubDate>Tue, 21 Apr 2026 15:13:37</pubDate>
			<category>Geophysical Research Letters</category>
		</item>
		<item>
			<title>Evaluating snow depth measurements from ground-penetrating radar and airborne lidar in boreal forest and tundra environments during the NASA SnowEx 2023 campaign</title>
			<author>Holland-Goon, Kajsa; Bonnell, Randall; McGrath, Daniel; Baxter, W.; Meehan, Tate; Webb, Ryan; Larsen, Christopher; Marshall, Hans-Peter; Mason, Megan; Vuyovich, Carrie</author>
			<link>https://pubs.usgs.gov/publication/70275281</link>
			<description>Snow is a vital component of high-latitude terrestrial systems, but environmental factors (e.g., permafrost) and complex vegetation challenge the accurate measurement of key snowpack properties. We evaluated local-scale ground-penetrating radar (GPR) and large-scale airborne lidar retrievals of snow depth collected during the NASA SnowEx 2023 campaign in tundra and boreal forest environments in Alaska along 44 short (3–12 m) transects. Compared to in situ observations, we identified modest biases for GPR snow depths (bias &lt;0.03 m in tundra, +0.06 m in boreal forests) and larger biases for lidar snow depths in the boreal forests (–0.16 m). At the Upper Kuparuk-Toolik tundra site, lidar snow depths exhibited a small bias (–0.02 m), whereas the bias was much larger at the Arctic Coastal Plain tundra site (+0.19 m). For most sites, biases were primarily related to sub-snow vegetation, tussocks, and seasonally dynamic ground. However, we identified vertical alignment issues with the Arctic Coastal Plain lidar snow depth dataset that likely contributed to the higher bias. The complex ground surface and sub-snow vegetation in these environments present a challenge to established snow depth measurement methods, which needs to be considered when evaluating novel remote sensing approaches.</description>
			<pubDate>Mon, 27 Apr 2026 15:06:55</pubDate>
			<category>The Cryosphere</category>
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		<item>
			<title>A Bayesian hierarchical modeling approach for species diversity in ecology</title>
			<author>Qian, Song; Dufour, Mark; Jaffe, Sabrina; Hilling, Corbin; Hintz, William</author>
			<link>https://pubs.usgs.gov/publication/70275240</link>
			<description>&lt;p&gt;&lt;span&gt;Species diversity is the foundation of many ecological disciplines. This metric is often approximated using species richness and evenness, even though actual richness likely exceeds observations due to imperfect sampling methods. Estimating the “true” species richness, which includes identifying the number of missing species, has intrigued ecologists for decades. We adopted a parametric model that appeared in Fisher et al. (1943), which models the numbers of individuals from different species as random samples from a negative binomial distribution, and developed a Bayesian computational approach to directly estimate the distribution model parameters. The model parameters represent species abundance and evenness, and can be used to derive species richness. We evaluated our parametric approach using (1) a simulation study and (2) three historical data sets. Furthermore, we illustrated the hierarchical modeling approach to combine data from multiple parallel studies using a biannual fishery survey data set. Our parametric model formulation is computationally efficient, and the hierarchical structure facilitates embedding diversity estimation into broader application, such as assessing spatial and temporal trends in species diversity associated with environmental stressors. Additionally, because the two parameters of the negative binomial distribution model represent species abundance and evenness of a community, this parametric approach facilitates a deeper understanding of the ecological systems under study. The negative binomial distribution model works with a wide range of species frequency distribution types. As a result, our emphasis on a parametric model can help us characterize the structure of an ecosystem and provide a greater depth of ecologically meaningful information.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 24 Apr 2026 14:13:47</pubDate>
			<category>Ecological Informatics</category>
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		<item>
			<title>A practical decision tool for marine bird mortality assessments</title>
			<author>Harvey, Johanna; Ramey, Andrew; Avery-Gomm, Stephanie; Robertson, Gregory; Romano, Marc; Mullinax, Jennifer; Boldenow, Megan; Atkinson, Philip; Prosser, Diann</author>
			<link>https://pubs.usgs.gov/publication/70275730</link>
			<description>&lt;p&gt;&lt;span&gt;Given the rise in anthropogenic, environmental, and disease events contributing to marine bird mortality, there is a critical need to improve the rigor of mortality assessments. Deficits in data collection and mortality estimation can hinder a manager’s ability to document the scale of events and assess population level impacts. Therefore, to inform decisions required during activities, such as conservation status assessments or harvest management, organizations may choose to incorporate mortality assessments into response plans. Resources, capacity, and assets to assess mortality vary across jurisdictions (federal, state, Indigenous, local, etc.), and clear guidance to support mortality assessments is often unavailable or not clearly addressed. Here, we present a decision support tool to help managers identify and evaluate survey options to assess bird mortality in a diverse array of scenarios. The objective of the decision tool is to improve data collection and availability, which will increase the ability to estimate mortality robustly, given situation-specific attributes and constraints. This decision tool is designed to guide the response when a mortality event is initially encountered and offers suggestions for assessment and reporting procedures in the absence of other guidance or to complement existing protocols. The decision tool is also meant to inform decision making for response determination and resource allocation. The tool facilitates examination of options for further assessment and monitoring, which users determine by examining questions pertaining to species prioritization, determination of mortality minimum spatial extent, and the potential magnitude of impacts on affected species. Finally, identification of appropriate survey methods that address imperfect detection when a complete census is not possible are determined by exploring location, spatial and temporal extent, and the type of species affected. Ultimately, this decision tool aims to facilitate and improve the standardization of mortality assessments, equipping managers with a practical resource to navigate the decision-making process for marine bird mortality estimation.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Thu, 14 May 2026 14:01:51</pubDate>
			<category>Ornithological Applications</category>
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			<title>Hydrogeology, groundwater salinity distributions, and assessment of the effect of oil-production activities on groundwater in the Midway Valley area, western Kern County, San Joaquin Valley, California</title>
			<author>Gillespie, Janice; Gannon, Riley; Ball, Lyndsay; Warden, John; Everett, Rhett; Stephens, Michael</author>
			<link>https://pubs.usgs.gov/publication/70275246</link>
			<description>&lt;p&gt;&lt;span&gt;This study seeks to determine the effects of oil field produced water disposal operations and well mechanical integrity issues on groundwater quality in oil fields in the southwest San Joaquin Valley, California. Whereas previous studies used groundwater wells to study shallow aquifers outside the oil fields, this study demonstrates that future approaches may use oil well geophysical logs to map groundwater head gradients, create salinity profiles and document changes in salinity over time in oil field areas with sparse groundwater well data and at depths greater than 330 m. We also incorporate an analysis of well histories to determine potential effects of compromised wellbore seals on changes in aquifer quality that cannot be explained by water disposal practices. Water quality in the aquifers is naturally brackish across most of the area, with better quality groundwater occurring in the eastern part. Geophysical logs are used to determine salinity variations within aquifers including the depth at which TDS exceeds 10,000 mg/L. This depth ranges from 366 m in the northwest to approximately 1,500 m in the southeast. Oil well porosity logs are used to determine water table elevations. These logs indicate the water table slopes south-southeast, showing the predominant groundwater flow direction is from oil field disposal areas toward better quality groundwater east of the oil fields. Geophysical logs show formation resistivity near some disposal facilities has decreased over time, indicating the salinity of the aquifer has increased due to disposal of saline produced water in injection wells and ponds. Oil well history analysis suggests that increased salinity over time in water-saturated sand intervals &amp;gt;1.5 km from disposal facilities may be caused by mechanical failures and/or incomplete borehole seals in poorly constructed or abandoned wellbores prevalent throughout the study area—particularly wells drilled prior to 1930.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Fri, 24 Apr 2026 14:10:27</pubDate>
			<category>PLOS Water</category>
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			<title>Water volumes, heat flow, and solute discharge from Old Faithful Geyser eruptions, Yellowstone National Park, USA</title>
			<author>Hurwitz, Shaul; McCleskey, R. Blaine; Rudolph, Maxwell; Peek, Sara; Roth, David; Schott-Atkins, Melissa; Manga, Michael; Folz Donahue, Kiernan; Reed, Mara; Hungerford, Jefferson</author>
			<link>https://pubs.usgs.gov/publication/70275178</link>
			<description>&lt;p&gt;&lt;span&gt;The iconic Old Faithful Geyser in Yellowstone National Park, USA, has attracted a significant amount of research because of the relative regularity and impressive size of its eruptions. Numerous studies have included observations, measurements, and analyses that informed models of geyser eruptions. However, fundamental quantities, including the associated mass and heat discharged, remain poorly constrained. In April 2025 we measured the volume of water from 45 Old Faithful Geyser eruptions using a portable flume in an outflow channel and specific conductance measurements in the Firehole River. We used high-speed video to perform velocimetry, measured changes in water chemistry to calculate the volume of water evaporated along the outflow channels, and used thermodynamic calculations to estimate the volume of water erupted as steam and to quantify the geyser&apos;s heat output. The calculated average volume of water discharged by Old Faithful Geyser in each eruption is 27.9&amp;nbsp;±&amp;nbsp;9.4&amp;nbsp;m&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;, with no relation between eruption volume and the length of the preceding eruption interval. Video analysis of the eruption&apos;s liquid-dominated phase yields similar volumes of 21–30&amp;nbsp;m&lt;/span&gt;&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;. The calculated heat flow from the geyser is 2.2–2.4&amp;nbsp;MW and the average annual discharge of chloride, fluoride, and arsenic are 63 tons, 3.9 tons, and 241&amp;nbsp;kg, respectively. Average annual silica deposition rate on the geyser cone and along the outflow channels is 7 tons. This study provides a methodology for future studies at geysers worldwide and a baseline for monitoring future activity changes at Old Faithful.&lt;/span&gt;&lt;/p&gt;</description>
			<pubDate>Tue, 21 Apr 2026 15:01:47</pubDate>
			<category>Journal of Volcanology and Geothermal Research</category>
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