{"pageNumber":"651","pageRowStart":"16250","pageSize":"25","recordCount":184617,"records":[{"id":70208223,"text":"70208223 - 2020 - Progress in natural capital accounting for ecosystems","interactions":[],"lastModifiedDate":"2020-01-31T10:13:43","indexId":"70208223","displayToPublicDate":"2020-01-31T09:56:02","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Progress in natural capital accounting for ecosystems","docAbstract":"<p><span>Reversing the ongoing degradation of the planet's ecosystems requires timely and detailed monitoring of ecosystem change and uses. Yet, the System of National Accounts (SNA), first developed in response to the economic crisis of the 1930s and used by statistical offices worldwide to record economic activity (for example, production, consumption, and asset accumulation), does not make explicit either inputs from the environment to the economy or the cost of environmental degradation (</span><a id=\"xref-ref-1-1\" class=\"xref-bibr\" href=\"https://science.sciencemag.org/content/367/6477/514#ref-1\" data-mce-href=\"https://science.sciencemag.org/content/367/6477/514#ref-1\"><i>1</i></a><span>,&nbsp;</span><a id=\"xref-ref-2-1\" class=\"xref-bibr\" href=\"https://science.sciencemag.org/content/367/6477/514#ref-2\" data-mce-href=\"https://science.sciencemag.org/content/367/6477/514#ref-2\"><i>2</i></a><span>). Experimental Ecosystem Accounting (EEA), part of the System of Environmental-Economic Accounting (SEEA), has been developed to monitor and report on ecosystem change and use, using the same accounting approach, concepts, and classifications as the SNA (</span><a id=\"xref-ref-3-1\" class=\"xref-bibr\" href=\"https://science.sciencemag.org/content/367/6477/514#ref-3\" data-mce-href=\"https://science.sciencemag.org/content/367/6477/514#ref-3\"><i>3</i></a><span>). The EEA is part of the statistical community's response to move SNA measurement “beyond gross domestic product (GDP).” With the first generation of ecosystem accounts now published in 24 countries, and with a push to finalize a United Nations (UN) statistical standard for ecosystem accounting by 2021, we highlight key advances, challenges, and opportunities.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.aaz8901","usgsCitation":"Hein, L., Bagstad, K.J., Obst, C., Edens, B., Schenau, S., Castillo, G., Soulard, F., Brown, C., Driver, A., Bordt, M., Steurer, A., Harris, R., and Capparros, A., 2020, Progress in natural capital accounting for ecosystems: Science, v. 6477, no. 367, p. 514-515, https://doi.org/10.1126/science.aaz8901.","productDescription":"2 p.","startPage":"514","endPage":"515","ipdsId":"IP-108491","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":371803,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6477","issue":"367","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hein, Lars","contributorId":176849,"corporation":false,"usgs":false,"family":"Hein","given":"Lars","email":"","affiliations":[],"preferred":false,"id":781013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagstad, Kenneth J. 0000-0001-8857-5615 kjbagstad@usgs.gov","orcid":"https://orcid.org/0000-0001-8857-5615","contributorId":3680,"corporation":false,"usgs":true,"family":"Bagstad","given":"Kenneth","email":"kjbagstad@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":781012,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Obst, Carl","contributorId":176851,"corporation":false,"usgs":false,"family":"Obst","given":"Carl","email":"","affiliations":[],"preferred":false,"id":781014,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edens, Bram","contributorId":176850,"corporation":false,"usgs":false,"family":"Edens","given":"Bram","email":"","affiliations":[],"preferred":false,"id":781015,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schenau, Sjoerd","contributorId":222041,"corporation":false,"usgs":false,"family":"Schenau","given":"Sjoerd","email":"","affiliations":[{"id":27734,"text":"Statistics Netherlands","active":true,"usgs":false}],"preferred":false,"id":781016,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Castillo, Gem","contributorId":222042,"corporation":false,"usgs":false,"family":"Castillo","given":"Gem","email":"","affiliations":[{"id":40481,"text":"Resources, Environment and Economics Center for Studies, Philippines","active":true,"usgs":false}],"preferred":false,"id":781017,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Soulard, Francois","contributorId":211874,"corporation":false,"usgs":false,"family":"Soulard","given":"Francois","email":"","affiliations":[{"id":38339,"text":"Statistics Canada","active":true,"usgs":false}],"preferred":false,"id":781018,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Brown, Claire","contributorId":222043,"corporation":false,"usgs":false,"family":"Brown","given":"Claire","email":"","affiliations":[{"id":40482,"text":"UNEP-World Conservation Monitoring Centre","active":true,"usgs":false}],"preferred":false,"id":781019,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Driver, Amanda","contributorId":222044,"corporation":false,"usgs":false,"family":"Driver","given":"Amanda","email":"","affiliations":[{"id":40483,"text":"South African National Biodiversity Institute","active":true,"usgs":false}],"preferred":false,"id":781020,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bordt, Michael 0000-0001-5634-2294","orcid":"https://orcid.org/0000-0001-5634-2294","contributorId":222045,"corporation":false,"usgs":false,"family":"Bordt","given":"Michael","email":"","affiliations":[{"id":40484,"text":"UN Economic and Social Commission for Asia and the Pacific","active":true,"usgs":false}],"preferred":false,"id":781021,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Steurer, Anton","contributorId":222046,"corporation":false,"usgs":false,"family":"Steurer","given":"Anton","email":"","affiliations":[{"id":40485,"text":"Statistical Office of the European Union","active":true,"usgs":false}],"preferred":false,"id":781022,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Harris, Rocky","contributorId":222065,"corporation":false,"usgs":false,"family":"Harris","given":"Rocky","email":"","affiliations":[],"preferred":false,"id":781094,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Capparros, Alejandro","contributorId":222047,"corporation":false,"usgs":false,"family":"Capparros","given":"Alejandro","email":"","affiliations":[{"id":34335,"text":"Spanish National Research Council","active":true,"usgs":false}],"preferred":false,"id":781023,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70208466,"text":"70208466 - 2020 - Expert bioblitzes facilitate non-native fish tracking and interagency partnerships","interactions":[],"lastModifiedDate":"2020-03-11T15:32:23","indexId":"70208466","displayToPublicDate":"2020-01-31T09:40:48","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2655,"text":"Management of Biological Invasions","active":true,"publicationSubtype":{"id":10}},"title":"Expert bioblitzes facilitate non-native fish tracking and interagency partnerships","docAbstract":"Documenting the distribution and composition of non-native species populations can be challenging, especially when species cross jurisdictional boundaries that require interagency coordination. Herein I report the development of three tools that have been used in Florida over the past seven years to assist with tracking of non-native fishes: 1) an overarching organization to increase coordination and communication amongst stakeholders (Florida Non-Native Fish Action Alliance); 2) regularly-scheduled expert bioblitzes (Fish Slams); and 3) symposia (Fish Chats). Ten Fish Slams were held since 2012, which have included nearly 100 individuals from 20 organizations. Participants have sampled nearly 200 unique sites, capturing 36 non-native fish taxa. These activities have generated over 600 records for the U.S. Geological Survey’s Nonindigenous Aquatic Species database. Many specimens collected during Fish Slams are deposited into natural history museums or used by researchers. Informal interactions amongst colleagues working together in the field, at check-in meetings at the end of the day, and during more structured Fish Chat symposia allow members of various organizations to become acquainted, build trust, and share information and technology, which may then lead to professional collaborations. While this program is focused on non-native fish species in south Florida, I also discuss how the expert bioblitz may be adapted to suit other taxonomic groups and a variety of conservation needs.","language":"English","publisher":"REABIC","doi":"10.3391/mbi.2020.11.1.10","usgsCitation":"Schofield, P.J., 2020, Expert bioblitzes facilitate non-native fish tracking and interagency partnerships: Management of Biological Invasions, v. 11, no. 1, p. 139-154, https://doi.org/10.3391/mbi.2020.11.1.10.","productDescription":"16 p.","startPage":"139","endPage":"154","ipdsId":"IP-109058","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":457927,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.3391/mbi.2020.11.1.10","text":"Publisher Index Page"},{"id":372225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.7822265625,\n              25.08062377244484\n            ],\n            [\n              -80.013427734375,\n              25.08062377244484\n            ],\n            [\n              -80.013427734375,\n              26.59343927024179\n            ],\n            [\n              -81.7822265625,\n              26.59343927024179\n            ],\n            [\n              -81.7822265625,\n              25.08062377244484\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"1","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schofield, Pamela J. 0000-0002-8752-2797 pschofield@usgs.gov","orcid":"https://orcid.org/0000-0002-8752-2797","contributorId":168659,"corporation":false,"usgs":true,"family":"Schofield","given":"Pamela","email":"pschofield@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":782015,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70208591,"text":"70208591 - 2020 - Applications of correlative light and electron microscopy (CLEM) to organic matter in the North American shale petroleum systems","interactions":[],"lastModifiedDate":"2020-02-20T09:12:46","indexId":"70208591","displayToPublicDate":"2020-01-31T09:12:37","publicationYear":"2020","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"1","title":"Applications of correlative light and electron microscopy (CLEM) to organic matter in the North American shale petroleum systems","docAbstract":"<p>Scanning electron microscopy (SEM) has revolutionized our understanding of shale petroleum systems through microstructural characterization of dispersed organic matter (OM). However, due to the low atomic weight of carbon, all OM appears black in SEM (BSE image) regardless of differences in thermal maturity or OM type (kerogen types or solid bitumen). Traditional petrographic identification of OM uses optical microscopy, where reflectance (%Ro), form, relief and fluorescence can be used to discern OM types and thermal maturation stage. Unfortunately, most SEM studies of shale OM do not employ correlative optical techniques, leading to misidentifications or to the conclusion that all OM (i.e., kerogen and solid bitumen) is the same. To improve the accuracy of SEM identifications of dispersed OM in shale, this study used correlative light and electron microscopy (CLEM) to create optical and SEM images of OM in the same fields of view (500x magnification) under white light, blue light, secondary electron, and backscatter electron conditions. Samples (n=8) of varying thermal maturities and typical of the North American shale petroleum systems were used, including the Green River Mahogany Zone, Bakken Formation, Ohio Shale, Eagle Ford Formation, Barnett Formation, Haynesville Formation and Woodford Shale. The CLEM image sets demonstrate the importance of correlative microscopy by showing how easily OM can be misidentified when viewed by SEM alone. Without CLEM techniques, petrographic data from SEM such as observations of organic nano-porosity may be misinterpreted, resulting in false or ambiguous results and impairing an improved understanding of organic diagenesis and catagenesis.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Mudstone diagenesis: Research perspectives for shale hydrocarbon reservoirs, seals, and source rocks","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"AAPG","isbn":"9180891814252","usgsCitation":"Valentine, B.J., and Hackley, P.C., 2020, Applications of correlative light and electron microscopy (CLEM) to organic matter in the North American shale petroleum systems, chap. 1 <i>of</i> Mudstone diagenesis: Research perspectives for shale hydrocarbon reservoirs, seals, and source rocks, p. 1-18.","productDescription":"18 p.","startPage":"1","endPage":"18","ipdsId":"IP-093317","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":372446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":372421,"type":{"id":15,"text":"Index Page"},"url":"https://store.aapg.org/detail.aspx?id=1310"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Valentine, Brett J. 0000-0002-8678-2431 bvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-8678-2431","contributorId":3846,"corporation":false,"usgs":true,"family":"Valentine","given":"Brett","email":"bvalentine@usgs.gov","middleInitial":"J.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":782638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hackley, Paul C. 0000-0002-5957-2551 phackley@usgs.gov","orcid":"https://orcid.org/0000-0002-5957-2551","contributorId":592,"corporation":false,"usgs":true,"family":"Hackley","given":"Paul","email":"phackley@usgs.gov","middleInitial":"C.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":782677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70226997,"text":"70226997 - 2020 - Ecosystem-specific growth responses to climate pattern by a temperate freshwater fish","interactions":[],"lastModifiedDate":"2021-12-27T14:45:19.675432","indexId":"70226997","displayToPublicDate":"2020-01-31T08:42:41","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1456,"text":"Ecological Indicators","active":true,"publicationSubtype":{"id":10}},"title":"Ecosystem-specific growth responses to climate pattern by a temperate freshwater fish","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab010\" class=\"abstract author\" lang=\"en\"><div id=\"as010\"><p id=\"sp0010\">Somatic growth patterns among animal populations are maintained through complex processes that vary among ecosystems. Changes in growth patterns may be concomitant with changes in climate; however, understanding how growth will manifest among ecosystems is limited. Information embedded within fish hard-parts (i.e., otoliths, spines, vertebrae) can account for variation in growth patterns resulting from changing climate conditions. Channel catfish<span>&nbsp;</span><i>Ictalurus punctatus</i><span>&nbsp;</span>is a freshwater fish species widely distributed across North America with limited information regarding climate influences on growth and differences in climate-growth relations among ecological systems. We assessed growth (total length) response to changing climate conditions for channel catfish among three waterbody types—pit lakes, irrigation and power-generation reservoirs, and flood-control reservoirs in Nebraska, USA. We used linear mixed-effect models and an information theoretic approach to assess the relative strengths among competing hypotheses. The most supported linear mixed-effect model of channel catfish growth was a function of fish age and an interaction between waterbody type and growing-degree-day (GDD). A positive trend existed in GDD from 1990 through 2008 whereby the predicted increase in GDD among waterbody types ranged from 182 GDD to 189 GDD. The predicted change in channel catfish growth resulting from increased GDD ranged from 1% to 39% among waterbody types. Channel catfish population rate functions, thus, may not respond similarly to climate conditions across ecosystem types. Changes in climate variables may contribute to system-specific responses in population dynamics for channel catfish as well as other similar freshwater species. The establishment of relations between climate and growth variables for a freshwater generalist with a plastic diet and broad temperature tolerance serves as an indication of the breadth of responses possible for freshwater fishes under global changes in climate conditions.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.ecolind.2020.106130","usgsCitation":"Spurgeon, J.J., Pegg, M., Pope, K.L., and Xie, L., 2020, Ecosystem-specific growth responses to climate pattern by a temperate freshwater fish: Ecological Indicators, v. 112, 106130, 6 p., https://doi.org/10.1016/j.ecolind.2020.106130.","productDescription":"106130, 6 p.","ipdsId":"IP-106474","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":467300,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.ecolind.2020.106130","text":"Publisher Index 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,{"id":70209332,"text":"70209332 - 2020 - Habitat affinities and at-sea ranging behaviors among main Hawaiian Island seabirds: Breeding seabird telemetry, 2013–2016","interactions":[],"lastModifiedDate":"2020-04-01T08:39:57","indexId":"70209332","displayToPublicDate":"2020-01-31T08:36:24","publicationYear":"2020","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Habitat affinities and at-sea ranging behaviors among main Hawaiian Island seabirds: Breeding seabird telemetry, 2013–2016","docAbstract":"Recent Hawaiʻi state clean energy policy mandates and federal interest in developing offshore renewable energy resources have prompted unsolicited lease requests for offshore wind energy infrastructure (OWEI) to be located in ocean waters off Hawaiʻi. This study describing at-sea ranging behaviors for five seabirds was intended to provide new information on Hawaiian breeding seabird distribution at sea, habitat utilization, and ranging behaviors within near-island waters and throughout outer continental shelf (OCS) waters surrounding the main Hawaiian Islands (MHI). We also estimate the percentage of time the five study species spent flying at altitudes equivalent to an expected rotor-swept-zone (RSZ; 30–194 m) for an offshore wind turbine and discuss potential collision risk from OWEI to the seabirds studied here. The MHI supports important seabird breeding populations and individual seabirds can now be equipped with a wide-variety of data loggers and location tracking devices that can provide complex, high-resolution information on movement patterns at sea. In this study, we used GPS loggers and temperature-depth-recorders (TDRs) to examine the at-sea distributions and ranging behaviors of five abundantly breeding species in the MHI: Red-tailed Tropicbird, Laysan Albatross, Wedge-tailed Shearwater, Brown Booby, and Red-footed Booby. We tracked these breeding seabirds from 14 different sites throughout the MHI; study colonies were located on the main islands of Maui, Oʻahu, Kauaʻi, and on associated islets. We used the Residence in Space and Time (RST) algorithm to classify behavior into resting, transiting, and searching/foraging (Torres et al. 2017). We used GPS altitude measurements to examine species-specific flight height and to estimate time spent flying in the RSZ. We mapped rediscretized tracking data for seabirds at each study colony according to behavioral class and trip type (when applicable) using kernel density estimates. During 2014–2016, we obtained GPS and TDR data from 59 and 34 Red-tailed Tropicbirds, respectively. Taken together, individuals revealed a bimodal (short- [~3 h, <100 km range] and long- [>3 d, >800 km range]) trip foraging strategy. While ranging at sea, we estimated that Red-tailed Tropicbirds spend 70.6% (95% confidence interval [CI] 70.1–71.0%) of flight time in the RSZ. TDR data for tropicbirds was noisy and we could not reliably identify dives. During 2014 and 2016, we obtained GPS data from 35 Laysan Albatrosses nesting on Kauaʻi and Oʻahu. Individuals during the mid- to late-chick rearing period engaged in a bimodal short- (<6 d, <400 km range) and long- (>6 d, >2,000 km range) trip foraging strategy. While ranging at sea, we estimated that Laysan Albatrosses spend 2.57% (95% CI 2.50–2.64%) of flight time in the RSZ. During 2013–2015, we obtained GPS and TDR data from 313 and 55 Wedge-tailed Shearwaters, respectively. Considering all the data together, individuals revealed a multi-modal trip duration foraging strategy consisting of intra-day (<24 h, <100 km range), short (<4 d, ~200 km range), and long (>4 d, ~100–400 km range) trips. While ranging at sea, we estimated that Wedge-tailed Shearwaters spend 5.20% (95% CI 5.13–5.27%) of flight time in the RSZ. Wedge-tailed Shearwaters dove to a mean (± SD) depth of 1.78 ± 1.35 m (median = 1.38 m); the deepest dive recorded was to 10.06 m. The mean dive duration for Wedge-tailed Shearwaters was 3.12 ± 3.44 s (median = 1.80 s). During 2014–2015, we obtained GPS and TDR data from 42 and 37 Brown Boobies, respectively. Almost all foraging trips (97%) were single-day trips and we did not detect any bimodality in the distribution of single-day trip durations. Brown Boobies foraged relatively close to their colony (<60 km range) and focused their at-sea use in nearshore, coastal waters off Kauaʻi and Niʻihau. While foraging at sea, we estimated that Brown Boobies spend 3.41% (95% CI 3.16–3.67%) of flight time in the RSZ","language":"English","publisher":"BOEM","collaboration":"BOEM","usgsCitation":"Adams, J., Felis, J.J., and Czapanskiy, M., 2020, Habitat affinities and at-sea ranging behaviors among main Hawaiian Island seabirds: Breeding seabird telemetry, 2013–2016, viii, 111 p. .","productDescription":"viii, 111 p. 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0000-0002-6302-905X","orcid":"https://orcid.org/0000-0002-6302-905X","contributorId":207793,"corporation":false,"usgs":false,"family":"Czapanskiy","given":"Max","email":"","affiliations":[{"id":37635,"text":"San Fransciso State University","active":true,"usgs":false}],"preferred":false,"id":786136,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70208453,"text":"70208453 - 2020 - Estimating late 19th century hydrology in the Greater Everglades Ecosystem: An integration of paleoecologic data and models","interactions":[],"lastModifiedDate":"2020-02-11T07:40:36","indexId":"70208453","displayToPublicDate":"2020-01-31T07:37:52","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5738,"text":"Frontiers in Environmental Science","active":true,"publicationSubtype":{"id":10}},"title":"Estimating late 19th century hydrology in the Greater Everglades Ecosystem: An integration of paleoecologic data and models","docAbstract":"Determining hydrologic conditions prior to instrumental records is a challenge for restoration of freshwater ecosystems worldwide.  Paleoecologic data provide this information on past conditions and when these data are used to adjust hydrologic models, allow conditions to be hindcast that may not be directly estimated from the paleo-data alone. In this context, the paleo-data provide real-world estimates as input to the models.  Restoration of the Greater Everglades Ecosystem requires this understanding of the hydrology of the natural system prior to significant alterations due to water management and land use.  Large scale models such as the Natural Systems Model (NSM 4.6.2) have been used by the South Florida Water Management District and other agencies responsible for restoration to estimate past hydrologic conditions; however, these models typically portray a drier natural system for the beginning of the 20th century than what is indicated by paleoecologic analyses and historical data.  The purpose of this study is to estimate pre-20th century water levels, hydroperiods and flow in the freshwater wetlands of the Everglades by using pollen assemblage data in three sediment cores to adjust the Natural Systems Model.  This study is designed to further test estimates of flow through the Everglades derived from analysis of sediment cores collected in Florida Bay.  The results demonstrate that the NSM 4.6.2 underestimates water levels and hydroperiods in the Everglades compared to the paleo-adjusted NSM 4.6.2 model outputs.  Flow models that use the paleo-adjusted water levels as input indicate flow through Shark River Slough in the late 19th century was approximately two times flow between 1990 and 2000, and flow through Taylor Slough was approximately three times flow between 1990 and 2000.  The flow estimates derived from this study agree with the estimates derived from earlier studies using estuarine cores.  This integration of paleoecologic information and hydrologic models provides resource managers with the best available estimates of past conditions and allows them to set realistic targets for restoration of freshwater ecosystems.","language":"English","publisher":"Frontiers","doi":"10.3389/fenvs.2020.00003","usgsCitation":"Marshall, F.E., Bernhardt, C.E., and Wingard, G.L., 2020, Estimating late 19th century hydrology in the Greater Everglades Ecosystem: An integration of paleoecologic data and models: Frontiers in Environmental Science, v. 8, no. 3, 21 p., https://doi.org/10.3389/fenvs.2020.00003.","productDescription":"21 p.","ipdsId":"IP-099728","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":457934,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/fenvs.2020.00003","text":"Publisher Index Page"},{"id":372206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.58447265624999,\n              25.110471486223346\n            ],\n            [\n              -80.2716064453125,\n              25.110471486223346\n            ],\n            [\n              -80.2716064453125,\n              25.903703303407667\n            ],\n            [\n              -81.58447265624999,\n              25.903703303407667\n            ],\n            [\n              -81.58447265624999,\n              25.110471486223346\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"3","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2020-01-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Marshall, Frank E.","contributorId":222355,"corporation":false,"usgs":false,"family":"Marshall","given":"Frank","email":"","middleInitial":"E.","affiliations":[{"id":40533,"text":"Cetacean Logic Foundation","active":true,"usgs":false}],"preferred":false,"id":781946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernhardt, Christopher E. 0000-0003-0082-4731 cbernhardt@usgs.gov","orcid":"https://orcid.org/0000-0003-0082-4731","contributorId":2131,"corporation":false,"usgs":true,"family":"Bernhardt","given":"Christopher","email":"cbernhardt@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":781947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wingard, G. Lynn 0000-0002-3833-5207 lwingard@usgs.gov","orcid":"https://orcid.org/0000-0002-3833-5207","contributorId":605,"corporation":false,"usgs":true,"family":"Wingard","given":"G.","email":"lwingard@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":781945,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70208263,"text":"70208263 - 2020 - Throughfall reduction x fertilization: Deep soil water usage in a clay rich ultisol under loblolly pine in the Southeast USA","interactions":[],"lastModifiedDate":"2020-06-19T16:20:27.21759","indexId":"70208263","displayToPublicDate":"2020-01-31T07:06:58","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5860,"text":"Frontiers in Forests and Global Change","active":true,"publicationSubtype":{"id":10}},"title":"Throughfall reduction x fertilization: Deep soil water usage in a clay rich ultisol under loblolly pine in the Southeast USA","docAbstract":"Forests in the Southeast USA are predicted to experience a moderate decrease in precipitation inputs over this century that may result in soil water deficiency during the growing season. The potential impact of a drier climate on the productivity of managed loblolly pine (Pinus taeda L.) plantations in the Southeast USA is uncertain. Access to water reserves in deep soil during drought periods may help buffer these forests from the effects of water deficits. To better understand the potential impact of drought on deep soil water, we studied the combined effects of throughfall reduction and fertilization on soil water usage in a clay rich Piedmont Ultisol to a depth of 3 m. In a 6-year-old loblolly pine plantation, we applied a throughfall reduction treatment (ambient vs. ~30% throughfall reduction) and a fertilization treatment (no fertilization vs. fertilization). Over 28 months, throughfall reduction lowered soil moisture for all depths and differences were significant in the surface soils (0–0.3 m) (1.2–3.6%) and deep soils (below 2 m) (2.6–3.6%). Fertilization also lowered soil moisture for all depths and differences were significant at 0.3–0.6 m (2.9%) and 1.94–3.06 m (4.5%). Fertilization when combined with the throughfall reduction treatment significantly decreased soil water at 0.1–0.9 m depth. Soils of all depths were rarely depleted of plant available water with the exception of 0–0.1 m, mainly during the growing season. Under throughfall reduction treatment, soil below 0.9 m consistently accounted for more than half of the change in plant available water during months when transpiration exceeded precipitation. When considering the whole soil profile in this clay rich Ultisol, soil water storage buffered transpirational demand in the face of decreasing throughfall input.","language":"English","publisher":"Frontiers","doi":"10.3389/ffgc.2019.00093","usgsCitation":"Qi, J., Markewitz, D.M., McGuire, M.A., Samuelson, L., and Ward, E., 2020, Throughfall reduction x fertilization: Deep soil water usage in a clay rich ultisol under loblolly pine in the Southeast USA: Frontiers in Forests and Global Change, v. 2, 93, 13 p., https://doi.org/10.3389/ffgc.2019.00093.","productDescription":"93, 13 p.","ipdsId":"IP-112050","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":457937,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3389/ffgc.2019.00093","text":"Publisher Index Page"},{"id":371901,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.130859375,\n              25.085598897064752\n            ],\n            [\n              -78.837890625,\n              25.085598897064752\n            ],\n            [\n              -78.837890625,\n              37.78808138412046\n            ],\n            [\n              -94.130859375,\n              37.78808138412046\n            ],\n            [\n              -94.130859375,\n              25.085598897064752\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"noUsgsAuthors":false,"publicationDate":"2020-01-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Qi, Jiaguo","contributorId":191352,"corporation":false,"usgs":false,"family":"Qi","given":"Jiaguo","email":"","affiliations":[],"preferred":false,"id":781188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Markewitz, Daniel M.","contributorId":222099,"corporation":false,"usgs":false,"family":"Markewitz","given":"Daniel","email":"","middleInitial":"M.","affiliations":[{"id":37470,"text":"University of Georgia, Athens","active":true,"usgs":false}],"preferred":false,"id":781189,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGuire, Mary Ann","contributorId":222100,"corporation":false,"usgs":false,"family":"McGuire","given":"Mary","email":"","middleInitial":"Ann","affiliations":[{"id":37470,"text":"University of Georgia, Athens","active":true,"usgs":false}],"preferred":false,"id":781190,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Samuelson, Lisa","contributorId":222101,"corporation":false,"usgs":false,"family":"Samuelson","given":"Lisa","email":"","affiliations":[{"id":13360,"text":"Auburn University","active":true,"usgs":false}],"preferred":false,"id":781191,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ward, Eric 0000-0002-5047-5464","orcid":"https://orcid.org/0000-0002-5047-5464","contributorId":167035,"corporation":false,"usgs":true,"family":"Ward","given":"Eric","email":"","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":781187,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70236098,"text":"70236098 - 2020 - SPEAR: The next generation GFDL modeling system for seasonal to multidecadal prediction and projection","interactions":[],"lastModifiedDate":"2022-08-29T11:53:33.588643","indexId":"70236098","displayToPublicDate":"2020-01-31T06:49:27","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5407,"text":"Journal of Advances in Modeling Earth Systems","active":true,"publicationSubtype":{"id":10}},"title":"SPEAR: The next generation GFDL modeling system for seasonal to multidecadal prediction and projection","docAbstract":"<div class=\"article-section__content en main\"><p>We document the development and simulation characteristics of the next generation modeling system for seasonal to decadal prediction and projection at the Geophysical Fluid Dynamics Laboratory (GFDL). SPEAR (<strong>S</strong>eamless System for<span>&nbsp;</span><strong>P</strong>rediction and<span>&nbsp;</span><strong>EA</strong>rth System<span>&nbsp;</span><strong>R</strong>esearch) is built from component models recently developed at GFDL—the AM4 atmosphere model, MOM6 ocean code, LM4 land model, and SIS2 sea ice model. The SPEAR models are specifically designed with attributes needed for a prediction model for seasonal to decadal time scales, including the ability to run large ensembles of simulations with available computational resources. For computational speed SPEAR uses a coarse ocean resolution of approximately 1.0° (with tropical refinement). SPEAR can use differing atmospheric horizontal resolutions ranging from 1° to 0.25°. The higher atmospheric resolution facilitates improved simulation of regional climate and extremes. SPEAR is built from the same components as the GFDL CM4 and ESM4 models but with design choices geared toward seasonal to multidecadal physical climate prediction and projection. We document simulation characteristics for the time mean climate, aspects of internal variability, and the response to both idealized and realistic radiative forcing change. We describe in greater detail one focus of the model development process that was motivated by the importance of the Southern Ocean to the global climate system. We present sensitivity tests that document the influence of the Antarctic surface heat budget on Southern Ocean ventilation and deep global ocean circulation. These findings were also useful in the development processes for the GFDL CM4 and ESM4 models.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2019MS001895","usgsCitation":"Delworth, T.L., Cooke, W.F., Adcroft, A.A., Bushuk, M., Chen, J., Dunne, K.A., Ginoux, P., Gudgel, R., Harris, L., Harrison, M.J., Hallberg, R.W., Johnson, N., Kapnick, S.B., Lin, S., Lu, F., Malyshev, S., Milly, P.C., Murakami, H., Naik, V., Pascale, S., Paynter, D., Rosati, A., Schwarzkopf, M.D., Shevliakova, E., Underwood, S., Wittenberg, A.T., Xiang, B., Yang, X., Zeng, F., Zhang, H., Zhang, L., and Zhao, M., 2020, SPEAR: The next generation GFDL modeling system for seasonal to multidecadal prediction and projection: Journal of Advances in Modeling Earth Systems, v. 12, no. 3, e2019MS001895, 36 p., https://doi.org/10.1029/2019MS001895.","productDescription":"e2019MS001895, 36 p.","ipdsId":"IP-106684","costCenters":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"links":[{"id":457939,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2019ms001895","text":"Publisher Index Page"},{"id":405782,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"3","noUsgsAuthors":false,"publicationDate":"2020-03-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Delworth, Thomas L.","contributorId":189909,"corporation":false,"usgs":false,"family":"Delworth","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":849991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooke, William F.","contributorId":295785,"corporation":false,"usgs":false,"family":"Cooke","given":"William","email":"","middleInitial":"F.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adcroft, Alistair A.","contributorId":295786,"corporation":false,"usgs":false,"family":"Adcroft","given":"Alistair","email":"","middleInitial":"A.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849993,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bushuk, Mitchell","contributorId":295787,"corporation":false,"usgs":false,"family":"Bushuk","given":"Mitchell","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849994,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chen, Jan-Huey","contributorId":295788,"corporation":false,"usgs":false,"family":"Chen","given":"Jan-Huey","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849995,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dunne, Krista A. 0000-0002-1220-6140 kadunne@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-6140","contributorId":203816,"corporation":false,"usgs":true,"family":"Dunne","given":"Krista","email":"kadunne@usgs.gov","middleInitial":"A.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":849997,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ginoux, Paul","contributorId":295789,"corporation":false,"usgs":false,"family":"Ginoux","given":"Paul","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849996,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gudgel, Richard","contributorId":295790,"corporation":false,"usgs":false,"family":"Gudgel","given":"Richard","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849998,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Harris, Lucas","contributorId":295792,"corporation":false,"usgs":false,"family":"Harris","given":"Lucas","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850000,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Harrison, Matthew J.","contributorId":295793,"corporation":false,"usgs":false,"family":"Harrison","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850001,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Hallberg, Robert W.","contributorId":295791,"corporation":false,"usgs":false,"family":"Hallberg","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":849999,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Johnson, Nathaniel","contributorId":295794,"corporation":false,"usgs":false,"family":"Johnson","given":"Nathaniel","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850002,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Kapnick, Sarah B.","contributorId":189908,"corporation":false,"usgs":false,"family":"Kapnick","given":"Sarah","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":850003,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Lin, Shian-Jian","contributorId":295795,"corporation":false,"usgs":false,"family":"Lin","given":"Shian-Jian","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850004,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Lu, Feiyu","contributorId":295796,"corporation":false,"usgs":false,"family":"Lu","given":"Feiyu","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850005,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Malyshev, Sergey","contributorId":189177,"corporation":false,"usgs":false,"family":"Malyshev","given":"Sergey","affiliations":[],"preferred":false,"id":850006,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Milly, Paul C. D. 0000-0003-4389-3139 cmilly@usgs.gov","orcid":"https://orcid.org/0000-0003-4389-3139","contributorId":176836,"corporation":false,"usgs":true,"family":"Milly","given":"Paul","email":"cmilly@usgs.gov","middleInitial":"C. D.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":false,"id":850007,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Murakami, Hiroyuki","contributorId":295797,"corporation":false,"usgs":false,"family":"Murakami","given":"Hiroyuki","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850008,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Naik, Vaishali","contributorId":295798,"corporation":false,"usgs":false,"family":"Naik","given":"Vaishali","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850009,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Pascale, Salvatore","contributorId":295799,"corporation":false,"usgs":false,"family":"Pascale","given":"Salvatore","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850010,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Paynter, David","contributorId":295801,"corporation":false,"usgs":false,"family":"Paynter","given":"David","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850011,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Rosati, Anthony","contributorId":295803,"corporation":false,"usgs":false,"family":"Rosati","given":"Anthony","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850012,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Schwarzkopf, M. D.","contributorId":295805,"corporation":false,"usgs":false,"family":"Schwarzkopf","given":"M.","email":"","middleInitial":"D.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850013,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Shevliakova, Elena","contributorId":201589,"corporation":false,"usgs":false,"family":"Shevliakova","given":"Elena","email":"","affiliations":[{"id":36211,"text":"GFDL/NOAA","active":true,"usgs":false}],"preferred":false,"id":850014,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Underwood, Seth","contributorId":201611,"corporation":false,"usgs":false,"family":"Underwood","given":"Seth","email":"","affiliations":[],"preferred":false,"id":850015,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Wittenberg, Andrew T.","contributorId":295809,"corporation":false,"usgs":false,"family":"Wittenberg","given":"Andrew","email":"","middleInitial":"T.","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850016,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Xiang, Baoqiang","contributorId":295812,"corporation":false,"usgs":false,"family":"Xiang","given":"Baoqiang","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850017,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Yang, Xiaosong","contributorId":201610,"corporation":false,"usgs":false,"family":"Yang","given":"Xiaosong","email":"","affiliations":[],"preferred":false,"id":850018,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Zeng, Fanrong","contributorId":295816,"corporation":false,"usgs":false,"family":"Zeng","given":"Fanrong","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850019,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"Zhang, Honghai","contributorId":295819,"corporation":false,"usgs":false,"family":"Zhang","given":"Honghai","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850020,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Zhang, Liping","contributorId":210614,"corporation":false,"usgs":false,"family":"Zhang","given":"Liping","email":"","affiliations":[],"preferred":false,"id":850021,"contributorType":{"id":1,"text":"Authors"},"rank":31},{"text":"Zhao, Ming","contributorId":295823,"corporation":false,"usgs":false,"family":"Zhao","given":"Ming","email":"","affiliations":[{"id":36803,"text":"NOAA","active":true,"usgs":false}],"preferred":false,"id":850022,"contributorType":{"id":1,"text":"Authors"},"rank":32}]}}
,{"id":70208526,"text":"70208526 - 2020 - Climate change vulnerability assessment for Pacific Lamprey in rivers of the Western United States","interactions":[],"lastModifiedDate":"2020-02-14T06:51:19","indexId":"70208526","displayToPublicDate":"2020-01-31T06:48:25","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Climate change vulnerability assessment for Pacific Lamprey in rivers of the Western United States","docAbstract":"Pacific Lamprey (Entosphenus tridentatus) are a native anadromous species that, like salmon, historically returned to spawn in large numbers in watersheds along the west coast of the United States (U.S.). Lamprey play a vital role in river ecosystems and are one of the oldest vertebrates that have persisted over time likely influencing the evolution of many aquatic species. Pacific Lamprey have declined in abundance and are restricted in distribution throughout Washington, Oregon, Idaho and California. A key uncertainty influencing Pacific Lamprey status is the impact of climate change. We modified the NatureServe Climate Change Vulnerability Index (CCVI) to accommodate climate predictions from the International Panel on Climate Change. Using downscaled information, we characterized changes in 15 rivers occupied by Pacific Lamprey in the western U.S. We evaluated this risk under Representative Concentration Pathways (RCP) 4.5 and 8.5 for two time periods (mid-century 2040–2069 and end-century 2070–2099). The CCVI scores generally increased when going from RCP 4.5 to RCP 8.5 in three Global Climate Models for both mid-century and end-century, which our analyses forecasts degraded stream temperature and hydrologic conditions under increasing greenhouse gas emissions. The geographically assessed results suggest that climate change impacts to Pacific Lamprey vulnerability are magnified in highly altered rivers. If we continue to observe greenhouse gas emission levels associated with the RCP 8.5, Pacific Lamprey will be at greater risk to climate change impacts. In order to mitigate the risk from climate change toward the end of the century, additional actions will need to be prioritized to rapidly reduce the impact of these threats such as increasing flow, creating backwater habitat, restoring riparian vegetation and reducing stream disturbances. The findings revealed the patterns of vulnerability for Pacific Lamprey across their U.S. range are informative for prioritizing river restoration actions when paired with regional implementation plans.","language":"English","publisher":"Taylor and Francis","doi":"10.1080/02705060.2019.1706652","usgsCitation":"Wang, C., Shaller, H.A., Coates, K.C., Hayes, M.C., and Rose, R.K., 2020, Climate change vulnerability assessment for Pacific Lamprey in rivers of the Western United States: Journal of Freshwater Ecology, v. 35, no. 1, p. 29-55, https://doi.org/10.1080/02705060.2019.1706652.","productDescription":"27 p.","startPage":"29","endPage":"55","ipdsId":"IP-113962","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":457941,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02705060.2019.1706652","text":"Publisher Index Page"},{"id":372336,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Washington, Oregon, Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.0244140625,\n              48.04870994288686\n            ],\n            [\n              -124.49707031249999,\n              44.77793589631623\n            ],\n            [\n              -124.49707031249999,\n              41.934976500546604\n            ],\n            [\n              -124.49707031249999,\n              40.38002840251183\n            ],\n            [\n              -123.96972656249999,\n              39.232253141714885\n            ],\n            [\n              -122.9150390625,\n              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and Wildlife Service, Retired","active":true,"usgs":false}],"preferred":false,"id":782297,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coates, Kelly C.","contributorId":193504,"corporation":false,"usgs":false,"family":"Coates","given":"Kelly","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":782298,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hayes, Michael C. 0000-0002-9060-0565 mhayes@usgs.gov","orcid":"https://orcid.org/0000-0002-9060-0565","contributorId":3017,"corporation":false,"usgs":true,"family":"Hayes","given":"Michael","email":"mhayes@usgs.gov","middleInitial":"C.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":782299,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rose, Robert K","contributorId":222492,"corporation":false,"usgs":false,"family":"Rose","given":"Robert","email":"","middleInitial":"K","affiliations":[{"id":40550,"text":"Yakama Nation Fisheries, Toppenish, WA","active":true,"usgs":false}],"preferred":false,"id":782300,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70208119,"text":"sir20195148 - 2020 - A system design for implementing advanced feature descriptions for a map knowledge base","interactions":[],"lastModifiedDate":"2020-01-31T06:30:23","indexId":"sir20195148","displayToPublicDate":"2020-01-30T17:09:24","publicationYear":"2020","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-5148","displayTitle":"A System Design for Implementing Advanced Feature Descriptions for a Map Knowledge Base","title":"A system design for implementing advanced feature descriptions for a map knowledge base","docAbstract":"<p>A prototype system to explore Linked Data that semantically integrates geospatial data in various formats from different publication sources with data from The National Map of the U.S. Geological Survey is presented. The focus is on accessing advanced feature descriptions for data from The National Map with data coreferenced from other sources. The prototype uses Geoserver to access The National Map data, which are converted to Resource Description Framework triples using Karma and stored in the Marmotta triplestore. Marmotta uses a Postgres relational database as a backend for the project and queries to the Marmotta triplestore are converted to structured query language and executed by Postgres. Triples retrieved are linked with same_as relationships to external data sources. The links to these sources provide additional attributes and relationships of the data from The National Map. Visualization of the results is provided using Leaflet and workflows for all parts of the system are defined. A use case for the system is provided to access structures and names information from The National Map for the Washington, D.C., area and link these to Geonames data, with visualization of the graphical and tabular results.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20195148","usgsCitation":"Wagner, M., Varanka, D.E., and Usery, E.L., 2020, A system design for implementing advanced feature descriptions for a map knowledge base: U.S. Geological Survey Scientific Investigations Report 2019–5148, 25 p., https://doi.org/10.3133/sir20195148. ","productDescription":"viii, 25 p.","numberOfPages":"38","onlineOnly":"Y","ipdsId":"IP-111001","costCenters":[{"id":5074,"text":"Center for Geospatial Information Science (CEGIS)","active":true,"usgs":true}],"links":[{"id":371735,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2019/5148/coverthb.jpg"},{"id":371736,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2019/5148/sir20195148.pdf","text":"Report","size":"3.00 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019–5148"}],"contact":"<p>Director, <a data-mce-href=\"https://www.usgs.gov/core-science-systems/ngp/ngtoc\" href=\"https://www.usgs.gov/core-science-systems/ngp/ngtoc\">National Geospatial Technical Operations Center</a><br>U.S. Geological Survey<br>1400 Independence Road<br>Rolla, MO 65401</p>","tableOfContents":"<ul><li>Foreword</li><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Background Knowledge</li><li>Data and Software</li><li>Preprocessing Workflow</li><li>Visualization Workflow</li><li>Advanced Feature Description Workflow</li><li>Example of a System Use Case</li><li>Discussion</li><li>Summary</li><li>References Cited</li><li>Glossary</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2020-01-30","noUsgsAuthors":false,"publicationDate":"2020-01-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Wagner, Matthew 0000-0002-3987-072X","orcid":"https://orcid.org/0000-0002-3987-072X","contributorId":221861,"corporation":false,"usgs":false,"family":"Wagner","given":"Matthew","affiliations":[{"id":40445,"text":"Student contractor to the U.S. Geological Survey","active":true,"usgs":false}],"preferred":false,"id":780557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Varanka, Dalia E. 0000-0003-2857-9600 dvaranka@usgs.gov","orcid":"https://orcid.org/0000-0003-2857-9600","contributorId":1296,"corporation":false,"usgs":true,"family":"Varanka","given":"Dalia","email":"dvaranka@usgs.gov","middleInitial":"E.","affiliations":[{"id":5074,"text":"Center for Geospatial Information Science (CEGIS)","active":true,"usgs":true},{"id":404,"text":"NGTOC Rolla","active":true,"usgs":true}],"preferred":true,"id":780556,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Usery, E. Lynn 0000-0002-2766-2173 usery@usgs.gov","orcid":"https://orcid.org/0000-0002-2766-2173","contributorId":231,"corporation":false,"usgs":true,"family":"Usery","given":"E.","email":"usery@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":780882,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207986,"text":"ofr20201008 - 2020 - Evaluation of survey methods for colonial waterbirds at Chase Lake National Wildlife Refuge, North Dakota","interactions":[],"lastModifiedDate":"2020-02-19T14:05:23","indexId":"ofr20201008","displayToPublicDate":"2020-01-30T17:08:14","publicationYear":"2020","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2020-1008","displayTitle":"Evaluation of Survey Methods for Colonial Waterbirds at Chase Lake National Wildlife Refuge, North Dakota","title":"Evaluation of survey methods for colonial waterbirds at Chase Lake National Wildlife Refuge, North Dakota","docAbstract":"<p>Estimating the number of breeding pairs in a mixed-species waterbird colony is difficult because colonial waterbirds are vulnerable to human intrusion and their colonies are often in remote areas with limited access. We investigated methods to estimate the number of nests of waterbirds at a large, mixed-species colony at Chase Lake National Wildlife Refuge in south-central North Dakota. The primary goals of this study were to evaluate survey methods for shrub- and ground-nesting colonial waterbirds at Chase Lake National Wildlife Refuge and to develop protocols for estimating abundance of the different species. The specific objectives were (1) to assess visible-nest counts for ciconiiform species from the perimeter of nesting areas (hereafter, perimeter counts) and observational surveys from fixed points outside the colony to count flights of adult ciconiiforms in and out of the colony (hereafter, flightline surveys) as alternatives to within-colony counts of ciconiiform nests, and (2) to assess semiautomated, pixel-based image-analysis techniques to estimate abundance of American White Pelicans (<i>Pelecanus erythrorhynchos</i>) as an alternative to traditional manual counts from aerial photographs.</p><p>For shrub-nesting ciconiiform species, observers counted 2,259 and 1,759 active ciconiiform nests in 2012 and 2013, respectively, during within-colony counts of ciconiiform nests. Results from within-colony counts of ciconiiform nests indicated a positive relation between the number of nests and the area of the shrub subcolony for the three most common ciconiiform species and all ciconiiform species combined. The perimeter nest counts of ciconiiform nests at Chase Lake represented only 18.8 percent of the total active ciconiiform nests counted in 11 subcolonies in 2012, which was well below the recommended target of 50 percent. Although we found a positive relationship between the number of nests counted during perimeter counts and the number of nests counted during within-colony counts for the three most common ciconiiform species and all ciconiiform species combined, perimeter counts at Chase Lake were hampered by disturbance to nesting birds. Thus, we discontinued the perimeter counts before they were completed. We did not develop predictive models from these perimeter counts in 2012 because these models could be misleading due to inconsistent application of the survey methods, which likely would have provided inaccurate perimeter counts. The extent of this issue is unknown. Flightline surveys at Chase Lake documented patterns of ciconiiform activity that were unknown for this region. For the common ciconiiform species, the number of flights to and from the South Island at Chase Lake were greatest in the morning (7:00−12:00 central daylight time [CDT]) and least in the afternoon (12:00−17:00), and least early in the breeding season (May 29–June 20, 2013) and greatest later in the breeding season (June 24–August 1, 2013). Flightline surveys are an index but lacked comparability with within-colony nest counts because the two methods provide measures of different things (that is, adult activity away from the colony as compared to the number of nests within the colony). The overall proportions of flights generally reflected the proportions of the within-colony nest counts for the four most common species: Black-crowned Night-Heron (<i>Nycticorax nycticorax</i>), Cattle Egret (<i>Bubulcus ibis</i>), Great Egret (<i>Ardea alba</i>), and Snowy Egret (<i>Egretta thula</i>). Flightline surveys at Chase Lake indicated apparent variation related to the time of day and season, as well as a variation in detection of inbound and outbound adult ciconiiforms. For ciconiiforms at Chase Lake, the most appropriate combination of survey approaches will depend on the need for annual estimates of nest abundance of ciconiiform species, balanced with the financial, personnel, and logistical constraints associated with the survey methods.</p><p>For ground-nesting American White Pelicans, the results from this study indicated that digital-image processing using remote-sensing software provides an accurate estimate of the number of American White Pelican nests. Estimates of the number of pelican nests from digital-image processing, using two commercially available remote-sensing software packages, produced nest estimates that were comparable to those of traditional manual counts from aerial photographs.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20201008","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service","usgsCitation":"Igl, L.D., Bartos, A.J., Woodward, R.O., Scherr, P., and Sovada, M.A, 2020, Evaluation of survey methods for colonial waterbirds at Chase Lake National Wildlife Refuge, North Dakota: U.S. Geological Survey Open-File Report 2020–1008, 44 p., https://doi.org/10.3133/ofr20201008. ","productDescription":"Report: viii, 44 p.; Data Release","numberOfPages":"56","onlineOnly":"Y","ipdsId":"IP-112516","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":371775,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2020/1008/ofr20201008.pdf","text":"Report","size":"7.63 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2020–1008"},{"id":371774,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2020/1008/coverthb.jpg"},{"id":371776,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P90NK31K","text":"USGS data release","description":"USGS Data Release","linkHelpText":"Evaluation of Survey Methods for Colonial Waterbirds at Chase Lake National Wildlife Refuge, North Dakota, data release"}],"country":"United States","state":"North Dakota ","otherGeospatial":"Chase Lake National Wildlife Refuge","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -99.481105,46.983794 ], [ -99.481105,47.030693 ], [ -99.417191,47.030693 ], [ -99.417191,46.983794 ], [ -99.481105,46.983794 ] ] ] } } ] }","contact":"<p>Director, <a data-mce-href=\"https://www.usgs.gov/centers/npwrc\" href=\"https://www.usgs.gov/centers/npwrc\">Northern Prairie Wildlife Research Center</a> <br>U.S. Geological Survey<br>8711 37th Street Southeast <br>Jamestown, North Dakota 58401</p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>History of Waterbird Monitoring at Chase Lake</li><li>Review of Potential Survey Methods at Chase Lake</li><li>Objectives</li><li>Study Area</li><li>Part A. Ciconiiforms Nesting in Tall Shrubs</li><li>Part B. Image Analysis of Nesting American White Pelicans</li><li>References</li><li>Appendix 1</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2020-01-30","noUsgsAuthors":false,"publicationDate":"2020-01-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Igl, Lawrence D. 0000-0003-0530-7266 ligl@usgs.gov","orcid":"https://orcid.org/0000-0003-0530-7266","contributorId":2381,"corporation":false,"usgs":true,"family":"Igl","given":"Lawrence","email":"ligl@usgs.gov","middleInitial":"D.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":780036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartos, Alisa J.","contributorId":221712,"corporation":false,"usgs":false,"family":"Bartos","given":"Alisa J.","affiliations":[{"id":40407,"text":"Northern Great Plains Joint Venture","active":true,"usgs":false}],"preferred":false,"id":780037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, Robert O.","contributorId":221713,"corporation":false,"usgs":false,"family":"Woodward","given":"Robert","email":"","middleInitial":"O.","affiliations":[{"id":12443,"text":"U.S. Geological Survey (retired)","active":true,"usgs":false}],"preferred":false,"id":780038,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scherr, Paulette","contributorId":221714,"corporation":false,"usgs":false,"family":"Scherr","given":"Paulette","email":"","affiliations":[{"id":36673,"text":"U.S. Fish and Wildlife Service (retired)","active":true,"usgs":false}],"preferred":false,"id":780039,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sovada, Marsha A.","contributorId":221715,"corporation":false,"usgs":false,"family":"Sovada","given":"Marsha","email":"","middleInitial":"A.","affiliations":[{"id":12443,"text":"U.S. Geological Survey (retired)","active":true,"usgs":false}],"preferred":false,"id":780040,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70208330,"text":"70208330 - 2020 - A geospatially resolved wetland vulnerability index: Synthesis of physical drivers","interactions":[],"lastModifiedDate":"2020-02-04T15:36:39","indexId":"70208330","displayToPublicDate":"2020-01-30T15:30:57","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"A geospatially resolved wetland vulnerability index: Synthesis of physical drivers","docAbstract":"Assessing wetland vulnerability to chronic and episodic physical drivers is fundamental\nfor establishing restoration priorities. We synthesized multiple data sets from E.B\nForsythe National Wildlife Refuge, New Jersey, to establish a wetland vulnerability\nmetric that integrates a range of physical processes, regulatory information and\nphysical/biophysical features. The geospatial data are based on aerial imagery, remote\nsensing, regulatory information, and hydrodynamic modeling, and include elevation,\ntidal range, unvegetated to vegetated marsh ratio (UVVR), shoreline erosion, potential\nexposure to contaminants, residence time, marsh condition change, change in salinity\nand salinity exposure, and sediment concentration. First, we delineated the wetland\ncomplex into individual marsh units based on surface contours and then defined a\nwetland vulnerability index that combined contributions from all parameters. We\napplied principal component and cluster analyses to explore the interrelations between\nthe data layers and separate regions that exhibited common characteristics. Our\nanalysis shows that the spatial variation of vulnerability in this domain cannot be\nexplained satisfactorily by a smaller subset of the variables. The most influential factor\non the vulnerability index was the combined effect of elevation, tide range, residence\ntime, and UVVR. Tide range and residence time had the highest correlation, and\nsimilar bay-wide spatial variation. Some variables (e.g., shoreline erosion) had no\nsignificant correlation with the rest of the variables. The aggregated index based on the\ncomplete dataset allows us to assess the overall state of a given marsh unit and quickly\nlocate the most vulnerable units in a larger marsh complex. The application of\ngeospatially complete datasets and consideration of chronic and episodic physical drivers\nrepresents an advance over traditional point-based methods for wetland assessment.","language":"English","publisher":"PLoS","doi":"10.1371/journal.pone.0228504","usgsCitation":"Defne, Z., Aretxabaleta, A., Ganju, N., Kalra, T., Jones, D.K., and Smith, K., 2020, A geospatially resolved wetland vulnerability index: Synthesis of physical drivers: PLoS ONE, v. 15, no. 1, e0228504, 27 p., https://doi.org/10.1371/journal.pone.0228504.","productDescription":"e0228504, 27 p.","ipdsId":"IP-109605","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":457943,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0228504","text":"Publisher Index Page"},{"id":372025,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","otherGeospatial":"E.B. Forsythe National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.476318359375,\n              39.37889504706486\n            ],\n            [\n              -74.0478515625,\n              39.37889504706486\n            ],\n            [\n              -74.0478515625,\n              40.1095880747414\n            ],\n            [\n              -74.476318359375,\n              40.1095880747414\n            ],\n            [\n              -74.476318359375,\n              39.37889504706486\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"1","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2020-01-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Defne, Zafer 0000-0003-4544-4310 zdefne@usgs.gov","orcid":"https://orcid.org/0000-0003-4544-4310","contributorId":5520,"corporation":false,"usgs":true,"family":"Defne","given":"Zafer","email":"zdefne@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781431,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aretxabaleta, Alfredo 0000-0002-9914-8018 aaretxabaleta@usgs.gov","orcid":"https://orcid.org/0000-0002-9914-8018","contributorId":140090,"corporation":false,"usgs":true,"family":"Aretxabaleta","given":"Alfredo","email":"aaretxabaleta@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781432,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ganju, Neil K. 0000-0002-1096-0465","orcid":"https://orcid.org/0000-0002-1096-0465","contributorId":202878,"corporation":false,"usgs":true,"family":"Ganju","given":"Neil K.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781434,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kalra, Tarandeep S. 0000-0001-5468-248X tkalra@usgs.gov","orcid":"https://orcid.org/0000-0001-5468-248X","contributorId":178820,"corporation":false,"usgs":true,"family":"Kalra","given":"Tarandeep S.","email":"tkalra@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":781433,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jones, Daniel K. 0000-0003-0724-8001 dkjones@usgs.gov","orcid":"https://orcid.org/0000-0003-0724-8001","contributorId":4959,"corporation":false,"usgs":true,"family":"Jones","given":"Daniel","email":"dkjones@usgs.gov","middleInitial":"K.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":781435,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Kathryn E.L. 0000-0002-7521-7875 kelsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-7521-7875","contributorId":173264,"corporation":false,"usgs":true,"family":"Smith","given":"Kathryn","email":"kelsmith@usgs.gov","middleInitial":"E.L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":781436,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70208398,"text":"70208398 - 2020 - Multi-decadal patterns of vegetation succession after tundra fire on the Yukon-Kuskokwim Delta, Alaska","interactions":[],"lastModifiedDate":"2020-02-09T13:41:53","indexId":"70208398","displayToPublicDate":"2020-01-30T13:39:46","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1562,"text":"Environmental Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Multi-decadal patterns of vegetation succession after tundra fire on the Yukon-Kuskokwim Delta, Alaska","docAbstract":"Alaska’s Yukon-Kuskokwim Delta (YKD) is one of the warmest parts of the\nArctic tundra biome and tundra fires are common in its upland areas. Here we combine\nfield measurements, Landsat observations, and quantitative cover maps for tundra plant\nfunctional types (PFTs) to characterize multi-decadal succession and landscape change\nafter fire in lichen-dominated upland tundra of the YKD, where extensive wildfires\noccurred in 1971–1972, 1985, 2006–2007, and 2015. Unburned tundra was\ncharacterized by abundant lichens and low lichen cover was consistently associated\nwith historical fire. While we observed some successional patterns that were consistent\nwith earlier work in Alaskan tussock tundra, other patterns were not. In the landscape\nwe studied, a large proportion of pre-fire moss cover and surface peat tended to survive\nfire, which favors survival of existing vascular plants and limits opportunities for seed\nrecruitment. Although shrub cover was much higher in 1985 and 1971–1972 burns than\nin unburned tundra, tall shrubs (>0.5 m height) were rare and the PFT maps indicate\nhigh landscape-scale variability in the degree and persistence of shrub increase after\nfire. Fire has induced persistent changes in species composition and structure of upland\ntundra on the YKD, but the lichen-dominated fuels and thick surface peat appear to\nhave limited the potential for severe fire and accompanying edaphic changes. Soil thaw\ndepths were about 10 cm deeper in 2006–2007 burns than in unburned tundra, but\nwere similar to unburned tundra in 1985 and 1971–1972 burns. Historically, repeat fire\nhas been rare on the YKD, and the functional diversity of vegetation has recovered\nwithin several decades post-fire. Our findings provide a basis for predicting and\nmonitoring post-fire tundra succession on the YKD and elsewhere.","language":"English","publisher":"IOPScience","doi":"10.1088/1748-9326/ab5f49","usgsCitation":"Frost, G., Loehman, R.A., Saperstein, L., Macander, M.J., Nelson, P., Paradis, D., and Natali, S.M., 2020, Multi-decadal patterns of vegetation succession after tundra fire on the Yukon-Kuskokwim Delta, Alaska: Environmental Research Letters, no. 2, 14 p., https://doi.org/10.1088/1748-9326/ab5f49.","productDescription":"14 p.","ipdsId":"IP-112003","costCenters":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true}],"links":[{"id":457945,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1088/1748-9326/ab5f49","text":"Publisher Index Page"},{"id":372177,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon-Kuskokwim Delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -167.958984375,\n              58.619777025081675\n            ],\n            [\n              -157.52197265625,\n              58.619777025081675\n            ],\n            [\n              -157.52197265625,\n              63.30281270313518\n            ],\n            [\n              -167.958984375,\n              63.30281270313518\n            ],\n            [\n              -167.958984375,\n              58.619777025081675\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","issue":"2","edition":"15","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationDate":"2020-01-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Frost, Gerald","contributorId":222261,"corporation":false,"usgs":false,"family":"Frost","given":"Gerald","email":"","affiliations":[{"id":40510,"text":"ABR, Inc","active":true,"usgs":false}],"preferred":false,"id":781726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loehman, Rachel A. 0000-0001-7680-1865 rloehman@usgs.gov","orcid":"https://orcid.org/0000-0001-7680-1865","contributorId":187605,"corporation":false,"usgs":true,"family":"Loehman","given":"Rachel","email":"rloehman@usgs.gov","middleInitial":"A.","affiliations":[{"id":118,"text":"Alaska Science Center Geography","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":false,"id":781725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saperstein, Lisa","contributorId":218974,"corporation":false,"usgs":false,"family":"Saperstein","given":"Lisa","email":"","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":781727,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Macander, Matthew J.","contributorId":203639,"corporation":false,"usgs":false,"family":"Macander","given":"Matthew","email":"","middleInitial":"J.","affiliations":[{"id":36669,"text":"ABR, Inc.—Environmental Research & Services","active":true,"usgs":false}],"preferred":false,"id":781728,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nelson, Peter","contributorId":198617,"corporation":false,"usgs":false,"family":"Nelson","given":"Peter","affiliations":[],"preferred":false,"id":781729,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Paradis, David","contributorId":222262,"corporation":false,"usgs":false,"family":"Paradis","given":"David","email":"","affiliations":[{"id":7063,"text":"University of Maine","active":true,"usgs":false}],"preferred":false,"id":781730,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Natali, Sue M.","contributorId":204028,"corporation":false,"usgs":false,"family":"Natali","given":"Sue","email":"","middleInitial":"M.","affiliations":[{"id":16705,"text":"Woods Hole Research Center","active":true,"usgs":false}],"preferred":false,"id":781731,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70207582,"text":"sir20195150 - 2020 - Numerical simulation of groundwater availability in central Moloka‘i, Hawai‘i","interactions":[],"lastModifiedDate":"2022-04-25T20:32:20.678493","indexId":"sir20195150","displayToPublicDate":"2020-01-30T12:22:46","publicationYear":"2020","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-5150","displayTitle":"Numerical Simulation of Groundwater Availability in Central Moloka‘i, Hawai‘i","title":"Numerical simulation of groundwater availability in central Moloka‘i, Hawai‘i","docAbstract":"<p>Since the 1990s, increased chloride concentrations of water pumped from wells (much of which is used for drinking water) and the effects of withdrawals on groundwater-dependent ecosystems have led to concerns over groundwater availability on the island of Molokaʻi, Hawaiʻi. An improved understanding of the hydrologic effects of proposed groundwater withdrawals is needed to ensure effective management of the groundwater resources of Molokaʻi, plan for possible growth, and accommodate cultural, social, and economic concerns. To address the information needs of managers and community stakeholders on Molokaʻi, the U.S. Geological Survey developed a numerical groundwater model capable of simulating salinity change and reduction in groundwater discharge in coastal areas of central and southern Molokaʻi. Estimates of groundwater recharge needed as input to the numerical groundwater model were made using a daily water budget for each decade during 1940−2012 (the period 2000−12 spanned 13 years) and the most current available data, including the distributions of monthly rainfall and potential evapotranspiration. Total island recharge during the decadal periods ranged from a low of about 189 Mgal/d during the 1970s to a high of 278 Mgal/d during the 1960s. These recharge estimates were used to develop an island-wide numerical groundwater model with simplifying assumptions (sharp interface between freshwater and saltwater; two-dimensional flow). The island-wide model provided estimates of groundwater inflows to the main area of interest simulated with a three-dimensional numerical groundwater model. Simulated withdrawal scenarios were selected in consultation with water managers and stakeholders and consisted of: (1) a baseline scenario using average recharge (1978−2007 rainfall and 2010 land cover) and average 2016−17 withdrawals; (2) a scenario using average recharge and withdrawals from existing wells at pending (as of January 2019) water-use permit rates; (3) six scenarios using average recharge and selected withdrawals from existing and proposed wells; and (4) a scenario using reduced recharge and selected withdrawals from existing and proposed wells. Results of the simulated withdrawal scenarios indicate that wells may be capable of producing groundwater with chloride concentrations below 250 mg/L at withdrawal rates exceeding average 2016−17 rates. However, the quality of water&nbsp;withdrawn from production wells is dependent on the rate and distribution of the withdrawals. For all nonbaseline scenarios, simulated groundwater discharge to the nearshore environment is reduced relative to the baseline scenario. Areas of discharge reduction may correspond to areas used for cultural or subsistence purposes. The three-dimensional numerical groundwater model developed for this study utilizes the latest available hydrologic and geologic information and is a useful tool for understanding the hydrologic effects of additional groundwater withdrawals in central Molokaʻi. The model has several limitations, including its nonuniqueness and inability to account for local-scale heterogeneities.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20195150","collaboration":"Prepared in cooperation with the State of Hawai‘i Department of Hawaiian Home Lands, State of Hawai‘i Office of Hawaiian Affairs, and County of Maui Department of Water Supply","usgsCitation":"Oki, D.S., Engott, J.A., and Rotzoll, K., 2020, Numerical simulation of groundwater availability in central Moloka‘i, Hawai‘i: U.S. Geological Survey Scientific Investigations Report 2019–5150, 95 p., https://doi.org/10.3133/sir20195150.","productDescription":"Report: ix, 95 p.; Data Release","numberOfPages":"95","onlineOnly":"Y","ipdsId":"IP-032683","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":399622,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_109628.htm"},{"id":371721,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9HRQASS","linkHelpText":"Central Molokaʻi, Hawaiʻi, SUTRA model"},{"id":371719,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2019/5150/coverthb.jpg"},{"id":371720,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2019/5150/sir20195150.pdf","text":"Report","size":"40 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019-5150"}],"country":"United States","state":"Hawaii","otherGeospatial":"Moloka‘i","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.77352905273438,\n              21.179289725795993\n            ],\n            [\n              -156.8572998046875,\n              21.163922551671376\n            ],\n            [\n              -156.92184448242188,\n              21.167764494849468\n            ],\n            [\n              -156.97265625,\n              21.211299542246586\n            ],\n            [\n              -156.99737548828125,\n              21.189533621502626\n            ],\n            [\n              -157.1429443359375,\n              21.199776807250093\n            ],\n            [\n              -157.21298217773435,\n              21.220261047755002\n            ],\n            [\n              -157.25830078125,\n              21.218980865996457\n            ],\n            [\n              -157.25555419921875,\n              21.17672864097083\n            ],\n            [\n              -157.2967529296875,\n              21.14599216495789\n            ],\n            [\n              -157.30499267578125,\n              21.097313035028538\n            ],\n            [\n              -157.18826293945312,\n              21.090906697412837\n            ],\n            [\n              -157.08801269531247,\n              21.103719096296263\n            ],\n            [\n              -157.03582763671875,\n              21.090906697412837\n            ],\n            [\n              -156.90811157226562,\n              21.051181240269393\n            ],\n            [\n              -156.84906005859375,\n              21.047336278183312\n            ],\n            [\n              -156.77215576171875,\n              21.08450008351735\n            ],\n            [\n              -156.70074462890625,\n              21.15879980561845\n            ],\n            [\n              -156.77352905273438,\n              21.179289725795993\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://mail.google.com/mail/?view=cm&amp;fs=1&amp;tf=1&amp;to=dc_hi@usgs.gov\" target=\"_blank\" rel=\"noopener\" data-mce-href=\"mailto:dc_hi@usgs.gov\">Director</a>,<br><a href=\"https://www.usgs.gov/piwsc\" data-mce-href=\"https://www.usgs.gov/piwsc\" target=\"_blank\" rel=\"noopener\">Pacific Islands Water Science Center</a><br><a href=\"https://www.usgs.gov/\" data-mce-href=\"https://www.usgs.gov/\" target=\"_blank\" rel=\"noopener\">U.S. Geological Survey</a><br>Inouye Regional Center<br>1845 Wasp Blvd., B176<br>Honolulu, HI 96818</p>","tableOfContents":"<p></p><ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Description of Study Area</li><li>Geology</li><li>Regional Groundwater-Flow System</li><li>Island-Wide Two-Dimensional Numerical Groundwater-Flow Model</li><li>Three-Dimensional Numerical Groundwater-Flow and Salinity Model</li><li>Simulation of Selected Withdrawal Scenarios</li><li>Limitations</li><li>Summary</li><li>References Cited</li><li>Appendixes</li></ul><p></p>","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"publishedDate":"2020-01-30","noUsgsAuthors":false,"publicationDate":"2020-01-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Oki, Delwyn S. 0000-0002-6913-8804","orcid":"https://orcid.org/0000-0002-6913-8804","contributorId":221122,"corporation":false,"usgs":true,"family":"Oki","given":"Delwyn","email":"","middleInitial":"S.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":778606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engott, John A. 0000-0003-1889-4519 jaengott@usgs.gov","orcid":"https://orcid.org/0000-0003-1889-4519","contributorId":1142,"corporation":false,"usgs":true,"family":"Engott","given":"John","email":"jaengott@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":778607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rotzoll, Kolja 0000-0002-5910-888X kolja@usgs.gov","orcid":"https://orcid.org/0000-0002-5910-888X","contributorId":3325,"corporation":false,"usgs":true,"family":"Rotzoll","given":"Kolja","email":"kolja@usgs.gov","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":false,"id":778608,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209711,"text":"70209711 - 2020 - Hawaiian hoary bat (Lasiurus cinereus semotus) acoustic monitoring at Hawaii Army National Guard (HIARNG) installations statewide","interactions":[],"lastModifiedDate":"2020-04-22T15:21:58.787089","indexId":"70209711","displayToPublicDate":"2020-01-30T10:15:35","publicationYear":"2020","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":5948,"text":"Hawaii Cooperative Studies Unit Technical Report Series","active":true,"publicationSubtype":{"id":4}},"displayTitle":"Hawaiian hoary bat (Lasiurus cinereus semotus) acoustic monitoring at Hawai`i Army National Guard (HIARNG) installations statewide","title":"Hawaiian hoary bat (Lasiurus cinereus semotus) acoustic monitoring at Hawaii Army National Guard (HIARNG) installations statewide","docAbstract":"Acoustic sampling for occurrence of the endangered Hawaiian hoary bat (Lasiurus cinereus semotus) was conducted at 18 “long-term” acoustic monitoring stations on 12 Hawai‘i Army National Guard (HIARNG) installations across the islands of Hawai‘i, Maui, Moloka‘i, O‘ahu, and Kaua‘i between 2012 and 2018. Bats were confirmed as present at 10 of these installations: Kealakekua Armory, Keaukaha Military Reservation (KMR), Hanapēpe Armory, Kekaha Firing Range (KFR), Pu‘unēnē Training Facility, Ukumehame Firing Range (UFR), Kaunakakai Armory, Bellows Regional Training Institute, Kalaeloa, Barber’s Point, and the 487th Military Parking Facility, Wahiawā. Seasonal frequency of bat detection was similar to previous acoustic studies for the islands of Hawai‘i, Maui, and O‘ahu. Hawaiian hoary bats were recorded at HIARNG installations during periods of pregnancy, lactation, and pup fledging. Our acoustic sampling did not record bat vocalizations at Fort Ruger and Waiawa Armory. Foraging activity was observed at nine acoustic monitoring stations on the islands of Hawai‘i, Kaua‘i, O‘ahu, and Maui. No foraging activity was observed on Moloka‘i and a single station on O‘ahu recorded one feeding buzz in September 2017 at Kalaeloa, Barber’s Point. Within-night detections showed bat activity was mostly confined to the first six hours of the night but was also variable among stations. In addition to long-term bat acoustic monitoring at HIARNG installations, Hawaiian hoary bat insect prey sampling with paired acoustic monitoring was conducted at KMR on Hawai‘i Island from May through August 2018. Insect abundance and bat activity were sampled within areas where goats and sheep were used to control weeds to determine if grazing by these ungulates attract and support potential prey for the insectivorous Hawaiian hoary bat. The assessment focused on types of flies that are often associated with livestock (muscoid flies, including house flies [Muscidae], blow flies [Calliphoridae], flesh flies [Sarcophagidae], and biting midges [Ceratopogonidae]), and moths that may be impacted by changes in the availability of grass. Insect abundance was found to vary in both space and time across the study area, with numbers of muscoid flies and biting midges increasing in the presence of livestock at some stations. Although these insects appeared to respond to livestock grazing in some instances, we did not find statistically significant responses in bat foraging as measured by echolocation activity between grazed stations and the ungrazed reference station. Thus, we found no evidence that suggested bats are drawn to foraging resources in grazed areas. This result may be influenced by several factors, including the size of Hawaiian hoary bat foraging ranges compared to the scale of study area, the type of ungulate and their dung, and the timing of insect activity. Hawaiian hoary bats use KMR and forage seasonally as evidenced by long-term acoustic studies and their presence in the ungulate grazing areas; however, the relatively small size of the ungulate herd and the area that they graze may not be able to support enough prey to have a significant influence on bat foraging rates.","largerWorkTitle":"","language":"English","publisher":"Hawai‘i Cooperative Studies Unit, University of Hawai‘i at Hilo","collaboration":"","usgsCitation":"Montoya-Aiona, K., Pinzari, C., Peck, R., Brinck, K.W., and Bonaccorso, F.J., 2020, Hawaiian hoary bat (Lasiurus cinereus semotus) acoustic monitoring at Hawaii Army National Guard (HIARNG) installations statewide: Hawaii Cooperative Studies Unit Technical Report Series, iv, 48 p.","productDescription":"iv, 48 p.","ipdsId":"IP-114220","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research 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,{"id":70270697,"text":"70270697 - 2020 - Assessing the spawning movement and habitat needs of riverine Neosho Smallmouth Bass","interactions":[],"lastModifiedDate":"2025-08-22T14:54:52.356995","indexId":"70270697","displayToPublicDate":"2020-01-30T09:47:06","publicationYear":"2020","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5373,"text":"Cooperator Science Series","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"CSS-145-2020","title":"Assessing the spawning movement and habitat needs of riverine Neosho Smallmouth Bass","docAbstract":"<p><span>Stream fishes are vulnerable to a variety of natural and anthropogenic stressors. Information on fish movements and habitat use is essential to conserve and manage populations, particularly at the edges of distributions and novel habitats. The Neosho Smallmouth Bass <i>Micropterus dolomieu velox</i> is endemic to the southwestern Ozark Highlands ecoregion, where the riverscape is highly dissected by impoundments. Our study objectives were to determine the pre-spawn, spawn, and post-spawn movements of adult, radio-tagged Neosho Smallmouth Bass, and identify the habitat factors at multiple spatial scales related to suitable spawning habitat. Movements by tagged fish in the Elk River of Oklahoma and Missouri and two Oklahoma tributaries draining to lower Elk River and Grand Lake O’ the Cherokee were greatest during the spring spawning period and were positively related to discharge and fish size; however, we observed considerable individual and stream-specific variability. Temperature and fish movement rate in the Elk River were positively related in all seasons except for winter, although temperature was less important for Smallmouth Bass movement in the smaller streams. Tagged fish were never detected using active or passive telemetry in the reservoir or reservoir-river interface except during periods of lotic character (i.e., the reservoir was not pooled above the Buffalo Creek-Elk River confluence). Nests were typically located at intermediate depths (mean = 0.8 m; SD = 0.3) and in low velocity habitats (0.0–0.2 m/s). Most of the nests examined comprised gravel substrates; however, 2.5% of the nests observed were located on full or partial bedrock substrate. We also documented nest clustering behavior by Neosho Smallmouth Bass (i.e., adjacent nests within 2 m of each other); 66 nest clusters were identified across 22 stream reaches. Cluster presence was more prevalent in warmer stream reaches with wide, shallow channels, and less likely in groundwater-gaining reaches, whereas overall nest abundance was greater in warmer streams and reaches with deeper pools. We showed the importance of both warmer streams and deep pools of small streams for Smallmouth Bass rearing (i.e., young-of-year abundance). We found negative relationships between floods and first-year juvenile survival and show the importance of stream network position (i.e., adjacency to larger streams) for mitigating the negative effects of July floods. Our analyses of both nesting and young-of-year habitat use suggest small streams, typically not considered important to many fisheries, are responsible for a proportion of Neosho Smallmouth Bass production. Further, consideration of management actions restricting take during the early spawning season may be warranted due to the unique nesting behavior (i.e., clustering) exhibited by this subspecies.</span></p>","language":"English","doi":"10.3996/css43006037","usgsCitation":"Brewer, S., and Miller, A., 2020, Assessing the spawning movement and habitat needs of riverine Neosho Smallmouth Bass: Cooperator Science Series CSS-145-2020, ii, 92 p., https://doi.org/10.3996/css43006037.","productDescription":"ii, 92 p.","ipdsId":"IP-115685","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":494517,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Missouri, Kansas, Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -95.13406967809759,\n              37.10685857731461\n            ],\n            [\n              -95.13406967809759,\n              36.131017076016235\n            ],\n            [\n              -94.4372095028383,\n              36.131017076016235\n            ],\n            [\n              -94.4372095028383,\n              37.10685857731461\n            ],\n            [\n              -95.13406967809759,\n              37.10685857731461\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationDate":"2022-09-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Brewer, Shannon K. 0000-0002-1537-3921","orcid":"https://orcid.org/0000-0002-1537-3921","contributorId":340552,"corporation":false,"usgs":true,"family":"Brewer","given":"Shannon K.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":946841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Andrew","contributorId":196361,"corporation":false,"usgs":false,"family":"Miller","given":"Andrew","affiliations":[],"preferred":false,"id":946842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70227149,"text":"70227149 - 2020 - Targeting aggregations of telemetered Lake Trout to increase gillnetting suppression efficacy","interactions":[],"lastModifiedDate":"2022-01-03T16:05:35.686916","indexId":"70227149","displayToPublicDate":"2020-01-30T08:40:54","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Targeting aggregations of telemetered Lake Trout to increase gillnetting suppression efficacy","docAbstract":"<p><span>Conserving Yellowstone Cutthroat Trout&nbsp;</span><i>Oncorhynchus clarkii bouvieri</i><span>&nbsp;by suppressing invasive Lake Trout&nbsp;</span><i>Salvelinus namaycush</i><span>&nbsp;in Yellowstone Lake is a high priority for Yellowstone National Park resource managers. Here, we tested whether targeting telemetered Lake Trout could increase the efficacy of Lake Trout suppression by gill netting. Mobile acoustic tracking surveys were performed to identify aggregations of tagged Lake Trout in summer (June–August) 2017. Lake Trout aggregations were relayed daily to suppression crews by phone, radio, or text and a printed map. Suppression crews set 30 large-mesh gill nets targeting telemetered Lake Trout aggregations (target treatment) and 124 large-mesh gill nets not targeting telemetered aggregations (nontarget treatment). Mean log</span><sub><i>e</i></sub><span>(CPUE) was higher for the target treatment (0.37; 95% credible interval [CRI]&nbsp;=&nbsp;0.08–0.65) than for the nontarget treatment (−0.37; 95% CRI&nbsp;=&nbsp;−0.51 to −0.21). Mean of the target treatment was higher than the mean of the nontarget treatment for over 99% of the 1,000 draws from the joint posterior distribution. Because of telemetry costs, mean CPUE per US$10,000 spent was similar between the target treatment (0.20; 95% CRI&nbsp;=&nbsp;0.15–0.26) and the nontarget treatment (0.15; 95% CRI&nbsp;=&nbsp;0.13–0.17). Telemetry is an effective strategy for improving Lake Trout CPUE, which corresponds to an increased efficiency in the Lake Trout suppression program.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/nafm.10401","usgsCitation":"Williams, J.R., Guy, C.S., Koel, T., and Bigelow, P.E., 2020, Targeting aggregations of telemetered Lake Trout to increase gillnetting suppression efficacy: North American Journal of Fisheries Management, v. 40, no. 1, p. 225-231, https://doi.org/10.1002/nafm.10401.","productDescription":"7 p.","startPage":"225","endPage":"231","ipdsId":"IP-107663","costCenters":[{"id":398,"text":"Montana Cooperative Fishery Research Unit","active":false,"usgs":true}],"links":[{"id":457948,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/nafm.10401","text":"Publisher Index Page"},{"id":393735,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone Lake, Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.58357238769531,\n              44.28502826057224\n            ],\n            [\n              -110.58357238769531,\n              44.57188260255312\n            ],\n            [\n              -110.19630432128906,\n              44.57188260255312\n            ],\n            [\n              -110.19630432128906,\n              44.28502826057224\n            ],\n            [\n              -110.58357238769531,\n              44.28502826057224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"40","issue":"1","noUsgsAuthors":false,"publicationDate":"2020-01-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Williams, Jacob R.","contributorId":270708,"corporation":false,"usgs":false,"family":"Williams","given":"Jacob","email":"","middleInitial":"R.","affiliations":[{"id":36244,"text":"MSU","active":true,"usgs":false}],"preferred":false,"id":829899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guy, Christopher S. 0000-0002-9936-4781 cguy@usgs.gov","orcid":"https://orcid.org/0000-0002-9936-4781","contributorId":2876,"corporation":false,"usgs":true,"family":"Guy","given":"Christopher","email":"cguy@usgs.gov","middleInitial":"S.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5062,"text":"Office of the Chief Scientist for Ecosystems","active":true,"usgs":true}],"preferred":true,"id":829799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koel, Todd M.","contributorId":270709,"corporation":false,"usgs":false,"family":"Koel","given":"Todd M.","affiliations":[{"id":36245,"text":"NPS","active":true,"usgs":false}],"preferred":false,"id":829900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bigelow, Patricia E.","contributorId":181861,"corporation":false,"usgs":false,"family":"Bigelow","given":"Patricia","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":829901,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209826,"text":"70209826 - 2020 - Climate relationships with increasing wildfire in the southwestern US from 1984 to 2015","interactions":[],"lastModifiedDate":"2020-04-30T12:22:10.730349","indexId":"70209826","displayToPublicDate":"2020-01-30T07:17:10","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Climate relationships with increasing wildfire in the southwestern US from 1984 to 2015","docAbstract":"Over the last several decades in forest and woodland ecosystems of the southwestern United States, wildfire size and severity have increased, thereby increasing the vulnerability of these systems to type conversions, invasive species, and other disturbances. A combination of land use history and climate change is widely thought to be contributing to the changing fire regimes. We examined climate-fire relationships in forest and woodland ecosystems from 1984 – 2015 in Arizona and New Mexico using 1) an expanded satellite-derived burn severity dataset that incorporates over one million additional burned hectares when compared to MTBS data, and 2) climate variables including temperature, precipitation, and vapor pressure deficit (VPD). Regional climate-fire relationships were assessed by correlating annual area burned, area burned at high and low severity, and percent high severity with fire season (May-August) and water-year (October-September) climate variables. We also analyzed relationships between climate and high-severity fire at the scale of the individual fires using a hurdle model. We found that increasing temperature and VPD and decreasing precipitation were associated with increasing area burned regionally, and that area burned at high severity had the strongest relationships with climate metrics. The relationship between climate and fire activity in the Southwest appears to be strengthening since 2000. VPD-fire correlations were consistently as strong as, or stronger than, temperature or precipitation variables alone, both regionally and at the scale of the individual fires. Notably, at the scale of the individual fires, temperature and precipitation were not significant predictors of fire activity. Thus, our results support the use of VPD as a more integrative climate metric to forecast fire activity. We suggest that the strong relationship between VPD and fire activity may be useful to assess the likelihood of high-severity fire occurrence through continued development of the high-severity fire threshold model we present. The link between increasing aridity and increasing wildfire activity suggests a future with more fire in Southwest forests and woodlands with projected warming, underscoring the urgency of restoration in dry forests to reduce the likelihood of uncharacteristic, large high-severity fires.","language":"English","publisher":"Elsevier","doi":"10.1016/j.foreco.2019.117861","collaboration":"","usgsCitation":"Mueller, S., Thode, A.E., Margolis, E.Q., Yocom, L., Young, J.M., and Iniguez, J.M., 2020, Climate relationships with increasing wildfire in the southwestern US from 1984 to 2015: Forest Ecology and Management, v. 460, no. , https://doi.org/10.1016/j.foreco.2019.117861.","productDescription":"117861, 14 p.","startPage":"","ipdsId":"IP-109702","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":457950,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index 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,{"id":70208207,"text":"70208207 - 2020 - Multi-region assessment of pharmaceutical exposures and predicted effects in USA wadeable urban-gradient streams","interactions":[],"lastModifiedDate":"2020-02-19T14:30:57","indexId":"70208207","displayToPublicDate":"2020-01-30T07:01:22","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2978,"text":"PLoS","active":true,"publicationSubtype":{"id":10}},"title":"Multi-region assessment of pharmaceutical exposures and predicted effects in USA wadeable urban-gradient streams","docAbstract":"Human-use pharmaceuticals in urban streams link aquatic-ecosystem health to human health. Pharmaceutical mixtures have been widely reported in larger streams due to historical emphasis on wastewater-treatment plant (WWTP) sources, with limited investigation of pharmaceutical exposures and potential effects in smaller headwater streams. In 2014–2017, the United States Geological Survey measured 111 pharmaceutical compounds in 308 headwater streams (261 urban-gradient sites sampled 3–5 times, 47 putative low-impact sites sampled once) in 4 regions across the US. Simultaneous exposures to multiple pharmaceutical compounds (pharmaceutical mixtures) were observed in 91% of streams (248 urban-gradient, 32 low-impact), with 88 analytes detected across all sites and cumulative maximum concentrations up to 36,142 ng/L per site. Cumulative detections and concentrations correlated to urban land use and presence/absence of permitted WWTP discharges, but pharmaceutical mixtures also were common in the 75% of sampled streams without WWTP. Cumulative exposure-activity ratios (EAR) indicated widespread transient exposures with high probability of molecular effects to vertebrates. Considering the potential individual and interactive effects of the detected pharmaceuticals and the recognized analytical underestimation of the pharmaceutical-contaminant (unassessed parent compounds, metabolites, degradates) space, these results demonstrate a nation-wide environmental concern and the need for watershed-scale mitigation of in-stream pharmaceutical contamination.","language":"English","publisher":"PLoS ","doi":"10.1371/journal.pone.0228214","usgsCitation":"Bradley, P., Journey, C., Button, D.T., Carlisle, D.M., Huffman, B.J., Qi, S.L., Romanok, K., and Van Metre, P.C., 2020, Multi-region assessment of pharmaceutical exposures and predicted effects in USA wadeable urban-gradient streams: PLoS, v. 1, no. 15, p. 1-25, https://doi.org/10.1371/journal.pone.0228214.","productDescription":"e0228214, 25 p.","startPage":"1","endPage":"25","ipdsId":"IP-108109","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":470,"text":"New Jersey 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,{"id":70208146,"text":"70208146 - 2020 - Passive seismic survey of sediment thickness, Dasht-e-Nawar basin, eastern Afghanistan","interactions":[],"lastModifiedDate":"2021-08-23T16:19:02.586487","indexId":"70208146","displayToPublicDate":"2020-01-29T20:10:02","publicationYear":"2020","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Passive seismic survey of sediment thickness, Dasht-e-Nawar basin, eastern Afghanistan","docAbstract":"Exploration of water resources is needed for public supply, extraction of mineral resources, and economic development in Afghanistan. Remotely-sensed data are useful for identifying the general nature of surface sediments, however, “boots on the ground” geophysical surveys or drilling programs are needed to quantify the thickness of sediments or aquifers. The nature of such investigations presents a risk to field crews that may prohibit exploration of potentially valuable aquifers or mineral resources. The Dasht-e-Nawar basin, in east-central Afghanistan, contains a 400 km2 playa that includes evaporative mineral deposits, particularly lithium, which has been of interest since the 1970s. However, exploration of the basin, as with many areas of Afghanistan, has been hampered by decades of conflict. In 2014, an investigation of the basin was conducted by the U.S. Department of Defense Task Force for Business and Stability Operations (TFBSO), and their contractor, in cooperation with the U.S. Geological Survey (USGS). For this investigation the USGS compared the results of a rapid passive seismic survey of basin sediment thickness to the results of an independently conducted gravity survey of the same area. \nEach point measurement for the passive seismic method requires less than 30 minutes in the field by one person. The technique utilizes ambient seismic noise without an external sound source such as required by traditional seismic surveys. Additionally, the technique does not require external sensor arrays, which can be kilometers long for some geophysical techniques. The passive seismic equipment used in this study weighs approximately 1 kilogram and is about 10 cm3 in size.  Although relatively new for assessment of sediment thickness, several investigations have found this method to be capable of estimating sediment thicknesses, in the 10’s to 1000 meter range, in settings with unconsolidated sediment over bedrock and a contrast in acoustic impedance. In this investigation, the gravity survey was conducted during a period of 3 weeks by an experienced field crew; required a detailed, centimeter-scale land elevation survey; and required laboratory analyses of sediment and rock densities to interpret the gravity data. In contrast, the passive seismic survey was collected by two inexperienced operators over a period of 8 days and required no additional data to interpret. Due to security restrictions, USGS personnel could not visit the site and the seismic operator was trained immediately prior to the field work. Although the quality of the seismic survey was affected by strong afternoon winds, and by the inexperience of the field operator, the results were fairly comparable to the gravity survey. Similar basin sediment thicknesses and patterns in sediment thickness were identified by both surveys in the basin with an estimated maximum thickness of approximately 170 m. The passive seismic technique required substantially less field resources and time than would be required by other geophysical surveys. Although this method will not be effective in all geologic settings, it may be a valuable assessment tool for use before conducting other, more intensive, geophysical efforts or drilling programs, especially in regions with elevated security risks such as Afghanistan.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Military Geoscience","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Springer","doi":"10.1007/978-3-030-32173-4_12","usgsCitation":"Mack, T., 2020, Passive seismic survey of sediment thickness, Dasht-e-Nawar basin, eastern Afghanistan, <i>in</i> Military Geoscience, p. 161-170, https://doi.org/10.1007/978-3-030-32173-4_12.","productDescription":"10 p.","startPage":"161","endPage":"170","ipdsId":"IP-071694","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":371788,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Afghanistan","otherGeospatial":"Dasht-e-Nawar basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              67.8955078125,\n              33.426856918285004\n            ],\n            [\n              67.8955078125,\n              33.74489664315623\n            ],\n            [\n              68.2086181640625,\n              33.74489664315623\n            ],\n            [\n              68.2086181640625,\n              33.426856918285004\n            ],\n            [\n              67.8955078125,\n              33.426856918285004\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2020-01-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Mack, Thomas J. 0000-0002-0496-3918","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":218727,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas J.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":780712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70208179,"text":"70208179 - 2020 - Cyanotoxin occurrence in large rivers of the United States","interactions":[],"lastModifiedDate":"2020-05-05T16:42:37.924675","indexId":"70208179","displayToPublicDate":"2020-01-29T19:57:48","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1999,"text":"Inland Waters","active":true,"publicationSubtype":{"id":10}},"title":"Cyanotoxin occurrence in large rivers of the United States","docAbstract":"Cyanotoxins occur in rivers worldwide but are understudied in lotic ecosystems relative to lakes and reservoirs. Eleven large river sites located throughout the United States were sampled during June–September 2017 to determine the occurrence of cyanobacteria with known cyanotoxin-producing strains, cyanotoxin synthetase genes, and cyanotoxins. Chlorophyll-a concentrations spanned the range from oligotrophic to eutrophic (0.5–64.4 µg L-1). Cyanobacteria were present in the algal communities of all rivers (82% of samples, n=50), but did not dominate the phytoplankton (0 to 52% of total abundance; mean=8.8%). Pseudanabaena and Planktothrix occurred most often and many (64%) of the cyanobacterial genera identified (n=25) have known cyanotoxin-producing strains. Cyanotoxin synthetase genes occurred in all but one river. The mcyE and sxtA genes were most common, present in 73% of rivers and 44% and 40% of samples, respectively. The cyrA gene was less common (22% of samples) but occurred in 64% of rivers. The anaC gene was detected in one river (4% of samples). Anatoxin-a and microcystins were detected at low levels (0.10–0.38 µg L-1) in two midcontinent rivers. Cylindrospermopsins and saxitoxins were not detected. Cyanobacteria, cyanotoxin synthetase genes, and cyanotoxins were present at low concentrations throughout this subset of US rivers. Eutrophic rivers located in the midcontinent region of the US had the highest algal biomass, abundance of cyanotoxin synthetase genes, and cyanotoxin occurrence.","language":"English","publisher":"Taylor and Francis ","doi":"10.1080/20442041.2019.1700749","usgsCitation":"Graham, J., Dubrovsky, N., Foster, G.M., King, L.R., Loftin, K., Rosen, B., and Stelzer, E., 2020, Cyanotoxin occurrence in large rivers of the United States: Inland Waters, v. 10, no. 1, p. 109-117, https://doi.org/10.1080/20442041.2019.1700749.","productDescription":"9 p.","startPage":"109","endPage":"117","ipdsId":"IP-108025","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":467301,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/20442041.2019.1700749","text":"Publisher Index Page"},{"id":437134,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9TID1VX","text":"USGS data release","linkHelpText":"Cyanotoxin, chlorophyll-a, and cyanobacterial toxin genetic data for samples collected at eleven large river sites throughout the United States, June through September 2017"},{"id":371752,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.6953125,\n              49.49667452747045\n            ],\n            [\n              -122.87109375,\n              49.095452162534826\n            ],\n            [\n              -122.87109375,\n              48.516604348867475\n            ],\n            [\n              -124.62890625,\n              48.40003249610685\n            ],\n            [\n              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jlgraham@usgs.gov","orcid":"https://orcid.org/0000-0002-6420-9335","contributorId":150737,"corporation":false,"usgs":true,"family":"Graham","given":"Jennifer L.","email":"jlgraham@usgs.gov","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":false,"id":780832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dubrovsky, Neil 0000-0001-7786-1149 nmdubrov@usgs.gov","orcid":"https://orcid.org/0000-0001-7786-1149","contributorId":221955,"corporation":false,"usgs":true,"family":"Dubrovsky","given":"Neil","email":"nmdubrov@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":780833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, Guy M. 0000-0002-9581-057X gfoster@usgs.gov","orcid":"https://orcid.org/0000-0002-9581-057X","contributorId":221956,"corporation":false,"usgs":true,"family":"Foster","given":"Guy","email":"gfoster@usgs.gov","middleInitial":"M.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":780834,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"King, Lindsey R.","contributorId":221957,"corporation":false,"usgs":false,"family":"King","given":"Lindsey","email":"","middleInitial":"R.","affiliations":[{"id":40462,"text":"USGS Kansas Water Science Center","active":true,"usgs":false}],"preferred":false,"id":780835,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Loftin, Keith 0000-0001-5291-876X kloftin@usgs.gov","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":221958,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","email":"kloftin@usgs.gov","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":780836,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rosen, Barry 0000-0002-8016-3939","orcid":"https://orcid.org/0000-0002-8016-3939","contributorId":221959,"corporation":false,"usgs":true,"family":"Rosen","given":"Barry","affiliations":[{"id":5064,"text":"Southeast Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":780837,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stelzer, Erin 0000-0001-7645-7603 eastelzer@usgs.gov","orcid":"https://orcid.org/0000-0001-7645-7603","contributorId":221960,"corporation":false,"usgs":true,"family":"Stelzer","given":"Erin","email":"eastelzer@usgs.gov","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":780838,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70209003,"text":"70209003 - 2020 - The community code verification exercise for simulating sequences of earthquakes and aseismic slip (SEAS)","interactions":[],"lastModifiedDate":"2020-03-10T18:40:26","indexId":"70209003","displayToPublicDate":"2020-01-29T18:36:01","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"The community code verification exercise for simulating sequences of earthquakes and aseismic slip (SEAS)","docAbstract":"Numerical simulations of sequences of earthquakes and aseismic slip (SEAS) have made\ngreat progress over past decades to address important questions in earthquake physics.\nHowever, significant challenges in SEAS modeling remain in resolving multiscale interactions\nbetween earthquake nucleation, dynamic rupture, and aseismic slip, and understanding\nphysical factors controlling observables such as seismicity and ground\ndeformation. The increasing complexity of SEAS modeling calls for extensive efforts\nto verify codes and advance these simulations with rigor, reproducibility, and broadened\nimpact. In 2018, we initiated a community code-verification exercise for SEAS simulations,\nsupported by the Southern California Earthquake Center. Here, we report the\nfindings from our first two benchmark problems (BP1 and BP2), designed to verify different\ncomputational methods in solving a mathematically well-defined, basic faulting\nproblem. We consider a 2D antiplane problem, with a 1D planar vertical strike-slip fault\nobeying rate-and-state friction, embedded in a 2D homogeneous, linear elastic halfspace.\nSequences of quasi-dynamic earthquakes with periodic occurrences (BP1) or\nbimodal sizes (BP2) and their interactions with aseismic slip are simulated. The comparison\nof results from 11 groups using different numerical methods show excellent agreements\nin long-term and coseismic fault behavior. In BP1, we found that truncated\ndomain boundaries influence interseismic stressing, earthquake recurrence, and coseismic\nrupture, and that model agreement is only achieved with sufficiently large domain\nsizes. In BP2, we found that complexity of fault behavior depends on how well physical\nlength scales related to spontaneous nucleation and rupture propagation are resolved.\nPoor numerical resolution can result in artificial complexity, impacting simulation results\nthat are of potential interest for characterizing seismic hazard such as earthquake size\ndistributions, moment release, and recurrence times. These results inform the development\nof more advanced SEAS models, contributing to our further understanding of\nearthquake system dynamics.","language":"English","publisher":"SSA","doi":"10.1785/0220190248","usgsCitation":"Erickson, B., Jiang, J., Barall, M., Lapusta, N., Dunham, E., Harris, R.A., Abrahams, L., Allison, K., Ampuero, J., Barbot, S., Cattania, C., Elbanna, A., Fialko, Y., Idini, B., Kozdon, J., Lambert, V., Liu, Y., Luo, Y., Ma, X., McKay, M.B., Segall, P., Shi, P., van den Ende, M., and Wei, M., 2020, The community code verification exercise for simulating sequences of earthquakes and aseismic slip (SEAS): Seismological Research Letters, v. 91, no. 2A, p. 874-890, https://doi.org/10.1785/0220190248.","productDescription":"17 p.","startPage":"874","endPage":"890","ipdsId":"IP-110929","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":457961,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hal.science/hal-03578332","text":"External Repository"},{"id":373083,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"2A","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2020-01-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Erickson, Brittany","contributorId":206382,"corporation":false,"usgs":false,"family":"Erickson","given":"Brittany","affiliations":[{"id":6929,"text":"Portland State University","active":true,"usgs":false}],"preferred":false,"id":784482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jiang, Junle","contributorId":206383,"corporation":false,"usgs":false,"family":"Jiang","given":"Junle","email":"","affiliations":[{"id":16619,"text":"UCSD","active":true,"usgs":false}],"preferred":false,"id":784483,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barall, Michael 0000-0001-7724-8563","orcid":"https://orcid.org/0000-0001-7724-8563","contributorId":198670,"corporation":false,"usgs":false,"family":"Barall","given":"Michael","affiliations":[],"preferred":false,"id":784484,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lapusta, Nadia","contributorId":223189,"corporation":false,"usgs":false,"family":"Lapusta","given":"Nadia","email":"","affiliations":[{"id":13711,"text":"Caltech","active":true,"usgs":false}],"preferred":false,"id":784485,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dunham, Eric","contributorId":204616,"corporation":false,"usgs":false,"family":"Dunham","given":"Eric","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":784486,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Harris, Ruth A. 0000-0002-9247-0768 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,{"id":70208161,"text":"70208161 - 2020 - Identification of Acara (Cichlidae: Cichlasoma) established in Florida, USA","interactions":[],"lastModifiedDate":"2020-03-11T14:43:12","indexId":"70208161","displayToPublicDate":"2020-01-29T18:25:24","publicationYear":"2020","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":994,"text":"BioInvasions Records","active":true,"publicationSubtype":{"id":10}},"title":"Identification of Acara (Cichlidae: Cichlasoma) established in Florida, USA","docAbstract":"<p><span>The Black Acara,&nbsp;</span><i>Cichlasoma bimaculatum</i><span>&nbsp;(Linnaeus, 1758), was first reported as introduced to Florida in 1965. Native to Venezuela, Guyana, Suriname, western French Guiana, and northern Brazil, the species is now distributed throughout Florida’s southern peninsula. Examination of live and preserved acara from Central Florida, heretofore identified as Black Acara, reveal the presence of an additional acara species, the Chanchita,&nbsp;</span><i>Cichlasoma dimerus</i><span>&nbsp;(Heckel, 1840). The Chanchita is native to Bolivia, Paraguay, Uruguay, southern Brazil, and northeastern Argentina. Despite similarities, Black Acara and Chanchita can be distinguished by number of anal-fin spines, body and fin color, caudal-fin pattern, and head, nape, and upper-flank scale-rim pigment. The Chanchita is established in multiple Central Florida drainages with the earliest known record from July 27, 2000. The Chanchita has not been found to co-occur with the Black Acara. The presence of Chanchita in more than one Central Florida spring and the widespread distribution of this previously unreported introduced species may be of concern to natural resource managers.</span></p>","language":"English","publisher":"REABIC","doi":"10.3391/bir.2020.9.1.18","usgsCitation":"Robins, R.H., Brown, M.E., and Crutchfield, R.A., 2020, Identification of Acara (Cichlidae: Cichlasoma) established in Florida, USA: BioInvasions Records, v. 9, no. 1, p. 133-145, https://doi.org/10.3391/bir.2020.9.1.18.","productDescription":"13 p.","startPage":"133","endPage":"145","ipdsId":"IP-110373","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":457964,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3391/bir.2020.9.1.18","text":"Publisher Index Page"},{"id":437135,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9RCXVLU","text":"USGS data 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