Use of eddy-covariance methods to "calibrate" simple estimators of evapotranspiration
David M. Sumner, Jeffrey S. Geurink, Amy Swancar
2017, Conference Paper, 2017 ASABE Annual International Meeting
Direct measurement of actual evapotranspiration (ET) provides quantification of this large component of the hydrologic budget, but typically requires long periods of record and large instrumentation and labor costs. Simple surrogate methods of estimating ET, if “calibrated†to direct measurements of ET, provide a reliable means to quantify ET. Eddy-covariance...
Response of deep groundwater to land use change in desert basins of the Trans-Pecos region, Texas, USA: Effects on infiltration, recharge, and nitrogen fluxes
Wendy Marie Robertson, J.K. Bohlke, John M. Sharp
2017, Hydrological Processes (31) 2349-2364
Quantifying the effects of anthropogenic processes on groundwater in arid regions can be complicated by thick unsaturated zones with long transit times. Human activities can alter water and nutrient fluxes, but their impact on groundwater is not always clear. This study of basins in the Trans-Pecos region of Texas links...
The U.S. Geological Survey Flagstaff Science Campus—Providing expertise on planetary science, ecology, water resources, geologic processes, and human interactions with the Earth
Robert J. Hart, R. Greg Vaughan, Kristin McDougall, Todd Wojtowicz, Prasad Thenkenbail
2017, Fact Sheet 2017-3051
The U.S. Geological Survey’s Flagstaff Science Campus is focused on interdisciplinary study of the Earth and solar system, and has the scientific expertise to detect early environmental changes and provide strategies to minimize possible adverse effects on humanity. The Flagstaff Science Campus (FSC) is located in Flagstaff, Arizona,...
On the probability distribution of daily streamflow in the United States
Annalise G. Blum, Stacey A. Archfield, Richard M. Vogel
2017, Hydrology and Earth System Sciences (21) 3093-3103
Daily streamflows are often represented by flow duration curves (FDCs), which illustrate the frequency with which flows are equaled or exceeded. FDCs have had broad applications across both operational and research hydrology for decades; however, modeling FDCs has proven elusive. Daily streamflow is a complex time series with flow values...
Daily reservoir sedimentation model: Case study from the Fena Valley Reservoir, Guam
Mathieu D. Marineau, Scott Wright
2017, Journal of Hydraulic Engineering (143)
A model to compute reservoir sedimentation rates at daily timescales is presented. The model uses streamflow and sediment load data from nearby stream gauges to obtain an initial estimate of sediment yield for the reservoir’s watershed; it is then calibrated to the total deposition calculated from repeat bathymetric surveys. Long-term...
Optimal hydrograph separation using a recursive digital filter constrained by chemical mass balance, with application to selected Chesapeake Bay watersheds
Jeff P. Raffensperger, Anna C. Baker, Joel D. Blomquist, Jessica A. Hopple
2017, Scientific Investigations Report 2017-5034
Quantitative estimates of base flow are necessary to address questions concerning the vulnerability and response of the Nation’s water supply to natural and human-induced change in environmental conditions. An objective of the U.S. Geological Survey National Water-Quality Assessment Project is to determine how hydrologic systems are affected by watershed characteristics,...
The Niobrara Formation as a challenge to water quality in the Arkansas River, Colorado, USA
Carleton R. Bern, Stogner
2017, Journal of Hydrology: Regional Studies (12) 181-195
Study regionArkansas River, east of the Rocky Mountains.Study focusCretaceous sedimentary rocks in the western United States generally pose challenges to water quality, often through mobilization of salts and trace metals by irrigation. However, in the Arkansas River Basin of Colorado, patchy exposure of multiple Cretaceous formations...
Selected water-resources activities of the U.S. Geological Survey in New England in 2017
Peter K. Weiskel
2017, Fact Sheet 2017-3049
The New England Water Science Center of the U.S. Geological Survey (USGS) is headquartered in Pembroke, New Hampshire, with offices in East Hartford, Connecticut; Augusta, Maine; Northborough, Massachusetts; and Montpelier, Vermont. The areas of expertise covered by the water science center’s staff of 130 include aquatic biology, chemistry, geographic information...
Widespread occurrence and potential for biodegradation of bioactive contaminants in Congaree National Park, USA
Paul M. Bradley, William A. Battaglin, Jimmy M. Clark, Frank Henning, Michelle L. Hladik, Luke R. Iwanowicz, Celeste A. Journey, Jeffrey W. Riley, Kristin M. Romanok
2017, Environmental Toxicology and Chemistry (36) 3045-3056
Organic contaminants with designed molecular bioactivity, such as pesticides and pharmaceuticals, originate from human and agricultural sources, occur frequently in surface waters, and threaten the structure and function of aquatic and terrestrial ecosystems. Congaree National Park in South Carolina (USA) is a vulnerable park unit due to its location downstream...
Challenges in recovering resources from acid mine drainage
D. Kirk Nordstrom, Robert J. Bowell, Kate M. Campbell, Charles N. Alpers
2017, Conference Paper, Mine water and circular economy
Metal recovery from mine waters and effluents is not a new approach but one that has occurred largely opportunistically over the last four millennia. Due to the need for low-cost resources and increasingly stringent environmental conditions, mine waters are being considered in a fresh light with a designed, deliberate approach...
Biological soil crusts: Diminutive communities of potential global importance
Scott Ferrenberg, Colin Tucker, Sasha C. Reed
2017, Frontiers in Ecology and the Environment (15) 160-167
Biological soil crusts (biocrusts) are widespread, diverse communities of cyanobacteria, fungi, lichens, and mosses living on soil surfaces, primarily in drylands. Biocrusts can locally govern primary production, soil fertility, hydrology, and surface energy balance, with considerable variation in these functions across alternate community states. Further, these communities have been implicated...
Hydrologic characterization of Bushy Park Reservoir, South Carolina, 2013–15
Paul Conrads, Matthew D. Petkewich, W. Fred Falls, Timothy H. Lanier
2017, Scientific Investigations Report 2017-5050
The Bushy Park Reservoir is a relatively shallow impoundment in a semi-tropical climate and is the principal water supply for the 400,000 people of the city of Charleston, South Carolina, and the surrounding areas including the Bushy Park Industrial Complex. Although there is an adequate supply of freshwater in the...
Sulfolobus islandicus meta-populations in Yellowstone National Park hot springs
Kate M. Campbell, Angela Kouris, Whitney England, Rika E. Anderson, R. Blaine McCleskey, D. Kirk Nordstrom, Rachel J. Whitaker
2017, Environmental Microbiology (19) 2334-2347
Abiotic and biotic forces shape the structure and evolution of microbial populations. We investigated forces that shape the spatial and temporal population structure of Sulfolobus islandicus by comparing geochemical and molecular analysis from seven hot springs in five regions sampled over 3 years in Yellowstone National Park. Through deep amplicon sequencing, we...
New distributional records of the stygobitic crayfish Cambarus cryptodytes (Decapoda: Cambaridae) in the Floridan Aquifer System of southwestern Georgia
Dante B. Fenolio, Matthew L. Niemiller, Andrew G. Gluesenkamp, Anna M. McKee, Steven J. Taylor
2017, Southeastern Naturalist (16) 163-181
Cambarus cryptodytes (Dougherty Plain Cave Crayfish) is an obligate inhabitant of groundwater habitats (i.e., a stygobiont) with troglomorphic adaptations in the Floridan aquifer system of southwestern Georgia and adjacent Florida panhandle, particularly in the Dougherty Plain and Marianna Lowlands. Documented occurrences of Dougherty Plain Cave Crayfish are spatially distributed as 2...
A multi-scale evaluation of pack stock effects on subalpine meadow plant communities in the Sierra Nevada
Steven R. Lee, Eric L. Berlow, Steven M. Ostoja, Matthew L. Brooks, Alexandre Génin, John R. Matchett, Stephen C. Hart
2017, PLoS ONE (12) 1-20
We evaluated the influence of pack stock (i.e., horse and mule) use on meadow plant communities in Sequoia and Yosemite National Parks in the Sierra Nevada of California. Meadows were sampled to account for inherent variability across multiple scales by: 1) controlling for among-meadow variability by using remotely sensed hydro-climatic...
Prediction of spatially explicit rainfall intensity–duration thresholds for post-fire debris-flow generation in the western United States
Dennis M. Staley, Jacquelyn Negri, Jason W. Kean, Jayme L. Laber, Anne C. Tillery, Ann M. Youberg
2017, Geomorphology (278) 149-162
Early warning of post-fire debris-flow occurrence during intense rainfall has traditionally relied upon a library of regionally specific empirical rainfall intensity–duration thresholds. Development of this library and the calculation of rainfall intensity-duration thresholds often require several years of monitoring local rainfall and hydrologic response to rainstorms, a time-consuming approach where...
Transient electromagnetic soundings in the San Luis Valley, Colorado, near the Great Sand Dunes National Park and Preserve and the Alamosa National Wildlife Refuge (field seasons 2007, 2009, and 2011)
David V. Fitterman
2017, Data Series 1043
Transient electromagnetic (TEM) soundings were made in the San Luis Valley, Colorado, to map the location of a blue clay unit as well as to investigate the presence of suspected faults. A total of 147 soundings were made near and in Great Sand Dunes National Park and Preserve, and an...
Five hydrologic and landscape databases for selected National Wildlife Refuges in the Southeastern United States
Gary R. Buell, Laura N. Gurley, Daniel L. Calhoun, Alexandria M. Hunt
2017, Open-File Report 2017-1018
This report serves as metadata and a user guide for five out of six hydrologic and landscape databases developed by the U.S. Geological Survey, in cooperation with the U.S. Fish and Wildlife Service, to describe data-collection, data-reduction, and data-analysis methods used to construct the databases and provides statistical and graphical...
A geochemical examination of humidity cell tests
Ann Maest, D. Kirk Nordstrom
2017, Applied Geochemistry (81) 109-131
Humidity cell tests (HCTs) are long-term (20 to >300 weeks) leach tests that are considered by some to be the among the most reliable geochemical characterization methods for estimating the leachate quality of mined materials. A number of modifications have been added to the original HCT method, but the interpretation...
Performance measures for a Mississippi River reintroduction into the forested wetlands of Maurepas Swamp
Ken W. Krauss, Gary P. Shaffer, Richard F. Keim, Jim L. Chambers, William B. Wood, Stephen B. Hartley
2017, Scientific Investigations Report 2017-5036
The use of freshwater diversions (river reintroductions) from the Mississippi River as a restoration tool to rehabilitate Louisiana coastal wetlands has been promoted widely since the first such diversion at Caernarvon became operational in the early 1990s. To date, aside from the Bonnet Carré Spillway (which is designed and operated...
Collecting a better water-quality sample: Reducing vertical stratification bias in open and closed channels
William R. Selbig
2017, Conference Paper, Proceedings of the 5th Federal Interagency Hydrologic Modeling Conference and the 10th Federal Interagency Sedimentation Conference
Collection of water-quality samples that accurately characterize average particle concentrations and distributions in channels can be complicated by large sources of variability. The U.S. Geological Survey (USGS) developed a fully automated Depth-Integrated Sample Arm (DISA) as a way to reduce bias and improve accuracy in water-quality concentration data. The DISA...
Hydrogeologic framework and hydrologic conditions of the Piney Point aquifer in Virginia
E. Randolph McFarland
2017, Scientific Investigations Report 2017-5041
The Piney Point aquifer in Virginia is newly described and delineated as being composed of six geologic units, in a study conducted by the U.S. Geological Survey in cooperation with the Virginia Department of Environmental Quality (VA DEQ). The eastward-dipping geologic units include, in stratigraphically ascending order, thesand of the...
Variability of dissolved organic carbon in precipitation during storms at the Shale Hills Critical Zone Observatory
Lidiia Iavorivska, Elizabeth W. Boyer, Jeffrey W. Grimm, Matthew P. Miller, David R. DeWalle, Kenneth J. Davis, Margot W. Kaye
2017, Hydrological Processes (31) 2935-2950
Organic compounds are removed from the atmosphere and deposited to the earth's surface via precipitation. In this study, we quantified variations of dissolved organic carbon (DOC) in precipitation during storm events at the Shale Hills Critical Zone Observatory, a forested watershed in central Pennsylvania (USA). Precipitation samples were collected consecutively...
Snow and ice
Jeremy S. Littell, Stephanie A. McAfee, Shad O’Neel, Louis C. Sass, Evan Burgess, Steve Colt, Paul Clark
Gregory D. Hayward, Steve Colt, Monica L. McTeague, Teresa N. Hollingsworth, editor(s)
2017, General Technical Report PNW-GTR-950-3
Temperature and precipitation are key determinants of snowpack levels. Therefore, climate change is likely to affect the role of snow and ice in the landscapes and hydrology of the Chugach National Forest region.Downscaled climate projections developed by Scenarios Network for Alaska and Arctic Planning (SNAP) are useful for examining projected...
How misapplication of the hydrologic unit framework diminishes the meaning of watersheds
James M. Omernik, Glenn E. Griffith, Robert M. Hughes, James B. Glover, Marc H. Weber
2017, Environmental Management (60) 1-11
Hydrologic units provide a convenient but problematic nationwide set of geographic polygons based on subjectively determined subdivisions of land surface areas at several hierarchical levels. The problem is that it is impossible to map watersheds, basins, or catchments of relatively equal size and cover the whole country. The hydrologic unit...