Thermal regimes of Rocky Mountain lakes warm with climate change
James Roberts, Kurt D. Fausch, Travis S. Schmidt, David M. Walters
2017, PLoS ONE (12) 1-17
Anthropogenic climate change is causing a wide range of stresses in aquatic ecosystems, primarily through warming thermal conditions. Lakes, in response to these changes, are experiencing increases in both summer temperatures and ice-free days. We used continuous records of lake surface temperature and air temperature to create statistical models of...
Reassessing rainfall in the Luquillo Mountains, Puerto Rico: Local and global ecohydrological implications
Sheila F. Murphy, Robert F. Stallard, Martha A. Scholl, Grizelle Gonzalez, Angel J. Torres-Sanchez
2017, PLoS ONE (12) 1-26
Mountains receive a greater proportion of precipitation than other environments, and thus make a disproportionate contribution to the world’s water supply. The Luquillo Mountains receive the highest rainfall on the island of Puerto Rico and serve as a critical source of water to surrounding communities. The area’s role as a...
Factors affecting marsh vegetation at the Liberty Island Conservation Bank in the Cache Slough region of the Sacramento–San Joaquin Delta, California
James L. Orlando, Judith Z. Drexler
2017, Open-File Report 2017-1077
The Liberty Island Conservation Bank (LICB) is a tidal freshwater marsh restored for the purpose of mitigating adverse effects on sensitive fish populations elsewhere in the region. The LICB was completed in 2012 and is in the northern Cache Slough region of the Sacramento–San Joaquin Delta. The wetland vegetation at...
Baseline assessments for coral reef community structure and demographics on West Maui
Bernardo Vargas-Angel, Darla White, Curt D. Storlazzi, Tova Callender, Paulo Maurin
2017, Report
The coastal and upslope terrains of West Maui have had a long history of impacts owing to more than a century of human activities. Resource extraction, agriculture, as well as residential and resort development have caused land-based pollution that impairs water quality and adversely impact the adjacent marine ecosystem. Today,...
Remote measurement of high preeruptive water vapor emissions at Sabancaya volcano by passive differential optical absorption spectroscopy
Christoph Kern, Pablo Masias, Fredy Apaza, Kevin Reath, Ulrich Platt
2017, Journal of Geophysical Research B: Solid Earth (122) 3540-3564
Water (H2O) is by far the most abundant volcanic volatile species and plays a predominant role in driving volcanic eruptions. However, numerous difficulties associated with making accurate measurements of water vapor in volcanic plumes have limited their use as a diagnostic tool. Here we present the first detection of water...
The difficulty of measuring the absorption of scattered sunlight by H2O and CO2 in volcanic plumes: A comment on Pering et al. “A novel and inexpensive method for measuring volcanic plume water fluxes at high temporal resolution,” Remote Sens. 2017, 9, 146
Christoph Kern
2017, Remote Sensing (9)
In their recent study, Pering et al. (2017) presented a novel method for measuring volcanic water vapor fluxes. Their method is based on imaging volcanic gas and aerosol plumes using a camera sensitive to the near-infrared (NIR) absorption of water vapor. The imaging data are empirically calibrated by comparison with...
How uncertainty analysis of streamflow data can reduce costs and promote robust decisions in water management applications
Hilary McMilan, Jan Seibert, Asgeir Petersen-Overleir, Michel Lang, Paul White, Ton Snelder, Kit Rutherford, Tobias Krueger, Robert R. Mason, Jr., Julie E. Kiang
2017, Water Resources Research (53) 5220-5228
Streamflow data are used for important environmental and economic decisions, such as specifying and regulating minimum flows, managing water supplies, and planning for flood hazards. Despite significant uncertainty in most flow data, the flow series for these applications are often communicated and used without uncertainty information. In this commentary, we...
Geomorphic processes responsible for decadal-scale arroyo changes, Rio Puerco, New Mexico
Allen C. Gellis, John G. Elliott, Milan Pavich
2017, Geological Society of America Bulletin (129) 1660-1680
The channel and arroyo of the Rio Puerco have continued to evolve since incision in the late 1800s. Resurveys of channel cross sections and aerial imagery over time indicate that between the 1970s and 1990s, the upstream reaches (type 1 morphology) of the Rio Puerco have continued to undergo construction...
Understanding and finding solutions to the problem of sedimentation in the National Wildlife Refuge System
Max Post van der Burg, Karen Jenni, Timothy L. Nieman, Josh D. Eash, Gregory A. Knutsen
2017, Journal of Fish and Wildlife Management (8) 648-660
The National Wildlife Refuge System (Refuge System) is a collection of public lands maintained by the U.S. Fish and Wildlife Service for migratory birds and other wildlife. Wetlands on individual National Wildlife Refuges (Refuges) may be at risk of increased sedimentation because of land use...
Monitoring water content dynamics of biological soil crusts
Michael H. Young, Lynn F. Fenstermaker, Jayne Belnap
2017, Journal of Arid Environments (142) 41-49
Biological soil crusts (hereafter, “biocrusts”) dominate soil surfaces in nearly all dryland environments. To better understand the influence of water content on carbon (C) exchange, we assessed the ability of dual-probe heat-pulse (DPHP) sensors, installed vertically and angled, to measure changes in near-surface water content. Four DPHP sensors were installed...
PeRL: A circum-Arctic Permafrost Region Pond and Lake database
Sina Muster, Kurt Roth, Moritz Langer, Stephan Lange, Fabio Cresto Aleina, Annett Bartsch, Anne Morgenstern, Guido Grosse, Benjamin M. Jones, A. B. K. Sannel, Ylva Sjoberg, Frank Gunther, Christian Andresen, Alexandra Veremeeva, Prajna R. Lindgren, Frederic Bouchard, Mark J. Lara, Daniel Fortier, Simon Charbonneau, Tarmo A. Virtanen, Gustaf Hugelius, J. Palmtag, Matthias B. Siewert, William J. Riley, Charles Koven, Julia Boike
2017, Earth System Science Data (9) 317-348
Ponds and lakes are abundant in Arctic permafrost lowlands. They play an important role in Arctic wetland ecosystems by regulating carbon, water, and energy fluxes and providing freshwater habitats. However, ponds, i.e., waterbodies with surface areas smaller than 1. 0 × 104 m2, have not been inventoried on global and regional scales. The Permafrost...
Microbial survival strategies in ancient permafrost: insights from metagenomics
Rachel Mackelprang, Alexander Burkert, Monica Haw, Tara Mahendrarajah, Christopher H. Conaway, Thomas A. Douglas, Mark P. Waldrop
2017, The ISME Journal (11) 2305-2318
In permafrost (perennially frozen ground) microbes survive oligotrophic conditions, sub-zero temperatures, low water availability and high salinity over millennia. Viable life exists in permafrost tens of thousands of years old but we know little about the metabolic and physiological adaptations to the challenges presented by life in frozen ground over...
Comparison of American Fisheries Society (AFS) standard fish sampling techniques and environmental DNA for characterizing fish communities in a large reservoir
Christina R. Perez, Scott A. Bonar, Jon J. Amberg, Bridget Ladell, Christopher B. Rees, William T. Stewart, Curtis J. Gill, Chris Cantrell, Anthony Robinson
2017, North American Journal of Fisheries Management (37) 1010-1027
Recently, methods involving examination of environmental DNA (eDNA) have shown promise for characterizing fish species presence and distribution in waterbodies. We evaluated the use of eDNA for standard fish monitoring surveys in a large reservoir. Specifically, we compared the presence, relative abundance, biomass, and relative percent composition of Largemouth Bass Micropterus...
Estimating the number of recreational anglers for a given waterbody
Kevin L. Pope, Larkin A. Powell, Brian S. Harmon, Mark A. Pegg, Christopher J. Chizinski
2017, Fisheries Research (191) 69-75
Knowing how many anglers use a given body of water is paramount for understanding components of a fishery related to angling pressure and harvest, yet no study has attempted to provide an estimate of the population size of anglers for a given waterbody. Here, we use information from creel surveys...
Heat as a groundwater tracer in shallow and deep heterogeneous media: Analytical solution, spreadsheet tool, and field applications
Barret L. Kurylyk, Dylan J. Irvine, Sean K. Carey, Martin A. Briggs, Dale D. Werkema, Mariah Bonham
2017, Hydrological Processes (31) 2648-2661
Groundwater flow advects heat, and thus, the deviation of subsurface temperatures from an expected conduction‐dominated regime can be analysed to estimate vertical water fluxes. A number of analytical approaches have been proposed for using heat as a groundwater tracer, and these have typically assumed a homogeneous medium. However, heterogeneous thermal...
Microbial-sized, carboxylate-modified microspheres as surrogate tracers in a variety of subsurface environments: An overview
Ronald W. Harvey, David W. Metge, Denis R. LeBlanc
2017, Procedia Earth and Planetary Science (17) 372-375
Since 1986, fluorescent carboxylate-modified polystyrene/latex microspheres (FCM) have been co-injected into aquifers along with conservative tracers and viruses, bacteria, and (or) protozoa. Use of FCM has resulted in new information about subsurface transport behaviors of microorganisms in fractured crystalline rock, karst limestone, soils, and granular aquifers. FCM have been used...
Fine particle retention within stream storage areas at base flow and in response to a storm event
J. D. Drummond, L. G. Larsen, R. González-Pinzón, A. I. Packman, Judson Harvey
2017, Water Resources Research (53) 5690-5705
Fine particles (1–100 µm), including particulate organic carbon (POC) and fine sediment, influence stream ecological functioning because they may contain or have a high affinity to sorb nitrogen and phosphorus. These particles are immobilized within stream storage areas, especially hyporheic sediments and benthic biofilms. However, fine particles are also known...
Estimating ages of Utah chubs by use of pectoral fin rays, otoliths, and scales
Kayla M Griffin, Zachary S. Beard, John M. Flinders, Michael C. Quist
2017, Western North American Naturalist (77) 189-194
Utah chub Gila atraria is native to the Upper Snake River system in Wyoming and Idaho and to the Lake Bonneville Basin in Utah and southeastern Idaho. However, the Utah chub has been introduced into many other waterbodies in the western United States, where it competes with ecologically and economically important species....
Landform features and seasonal precipitation predict shallow groundwater influence on temperature in headwater streams
Zachary C. Johnson, Craig D. Snyder, Nathaniel P. Hitt
2017, Water Resources Research (53) 5788-5812
Headwater stream responses to climate change will depend in part on groundwater‐surface water exchanges. We used linear modeling techniques to partition likely effects of shallow groundwater seepage and air temperature on stream temperatures for 79 sites in nine focal watersheds using hourly air and water temperature measurements collected during summer...
Life history migrations of adult Yellowstone Cutthroat Trout in the upper Yellowstone River
Brian D. Ertel, Thomas E. McMahon, Todd M. Koel, Robert E. Gresswell, Jason Burckhardt
2017, North American Journal of Fisheries Management (37) 743-755
Knowledge of salmonid life history types at the watershed scale is increasingly recognized as a cornerstone for effective management. In this study, we used radiotelemetry to characterize the life history movements of Yellowstone Cutthroat Trout Oncorhynchus clarkii bouvieri in the upper Yellowstone River, an extensive tributary that composes nearly half of the...
Nitrogenase activity by biological soil crusts in cold sagebrush steppe ecosystems
Stacy G. Schwabedissen, Kathleen A. Lohse, Sasha C. Reed, Ken A. Aho, Timothy S. Magnuson
2017, Biogeochemistry (134) 57-76
In drylands worldwide, biological soil crusts (BSC) form a thin photosynthetic cover across landscapes, and provide vital benefits in terms of stabilizing soil and fixing nitrogen (N) and carbon (C). Numerous studies have examined the effects of climate and disturbance on BSC functions; however, few have characterized these responses in...
Physical response of a back-barrier estuary to a post-tropical cyclone
Alexis Beudin, Neil Kamal Ganju, Zafer Defne, Alfredo Aretxabaleta
2017, Journal of Geophysical Research C: Oceans (122) 5888-5904
This paper presents a modeling investigation of the hydrodynamic and sediment transport response of Chincoteague Bay (VA/MD, USA) to Hurricane Sandy using the Coupled Ocean-Atmosphere-Wave-Sediment-Transport (COAWST) modeling system. Several simulation scenarios with different combinations of remote and local forces were conducted to identify the dominant physical processes. While 80% of...
Inputs and internal cycling of nitrogen to a causeway influenced, hypersaline lake, Great Salt Lake, Utah, USA
David L. Naftz
2017, Aquatic Geochemistry (23) 199-216
Nitrogen inputs to Great Salt Lake (GSL), located in the western USA, were quantified relative to the resident nitrogen mass in order to better determine numeric nutrient criteria that may be considered at some point in the future. Total dissolved nitrogen inputs from four surface-water sources entering GSL were modeled...
Downscaling wind and wavefields for 21st century coastal flood hazard projections in a region of complex terrain
Andrea C. O'Neill, Li H. Erikson, Patrick L. Barnard
2017, Earth and Space Science (4) 314-334
While global climate models (GCMs) provide useful projections of near-surface wind vectors into the 21st century, resolution is not sufficient enough for use in regional wave modeling. Statistically downscaled GCM projections from Multivariate Adaptive Constructed Analogues provide daily averaged near-surface winds at an appropriate spatial resolution for wave modeling within...
Numerical studies of depressurization-induced gas production from an interbedded marine turbidite gas hydrate reservoir model
Evgeniy Myshakin, Jeen-Shang Lin, Shun Uchida, Yongkoo Seol, Timothy S. Collett, Ray Boswell
2017, Conference Paper, Proceeding of the 9th International Conference on Gas Hydrates
The numerical simulation of thin hydrate-bearing sand layers interbedded with mud layers is investigated. In this model, the lowest hydrate layer occurs at the base of gas hydrate stability and overlies a thinly-interbedded saline aquifer. The predicted gas rates reach 6.25 MMscf/day (1.77 x 105 m3 /day) after 90 days...
