Groundwater connectivity of upland-embedded wetlands in the Prairie Pothole Region
Brian Neff, Donald O. Rosenberry
2018, Wetlands (38) 51-63
Groundwater connections from upland-embedded wetlands to downstream waterbodies remain poorly understood. In principle, water from upland-embedded wetlands situated high in a landscape should flow via groundwater to waterbodies situated lower in the landscape. However, the degree of groundwater connectivity varies across systems due to factors such as geologic setting, hydrologic...
Comparative analyses of hydrological responses of two adjacent watersheds to climate variability and change using the SWAT model
Sangchul Lee, In-Young Yeo, Ali M. Sadeghi, Gregory W. McCarty, Wells Hively, Megan W. Lang, Amir Sharifi
2018, Hydrology and Earth System Sciences (22) 689-708
Water quality problems in the Chesapeake Bay Watershed (CBW) are expected to be exacerbated by climate variability and change. However, climate impacts on agricultural lands and resultant nutrient loads into surface water resources are largely unknown. This study evaluated the impacts of climate variability and change on two adjacent watersheds...
Estimating wetland connectivity to streams in the Prairie Pothole Region: An isotopic and remote sensing approach
J. R. Brooks, David M. Mushet, Melanie K. Vanderhoof, Scott G. Leibowitz, J. R. Christensen, Brian Neff, Donald O. Rosenberry, W. D. Rugh, L.C. Alexander
2018, Water Resources Research (54) 955-977
Understanding hydrologic connectivity between wetlands and perennial streams is critical to understanding the reliance of stream flow on inputs from wetlands. We used the isotopic evaporation signal in water and remote sensing to examine wetland‐stream hydrologic connectivity within the Pipestem Creek watershed, North Dakota, a watershed dominated by prairie‐pothole wetlands....
Flood-inundation maps for the Withlacoochee River From Skipper Bridge Road to St. Augustine Road, within the City of Valdosta, Georgia, and Lowndes County, Georgia
Jonathan W. Musser
2018, Scientific Investigations Report 2018-5011
Digital flood-inundation maps for a 12.6-mile reach of the Withlacoochee River from Skipper Bridge Road to St. Augustine Road (Georgia State Route 133) were developed to depict estimates of the areal extent and depth of flooding corresponding to selected water levels (stages) at the U.S. Geological Survey (USGS) streamgage at...
Evaluation of the Radar Stage Sensor manufactured by Forest Technology Systems—Results of laboratory and field testing
Gerald A. Kunkle
2018, Open-File Report 2017-1085
Two identical Radar Stage Sensors from Forest Technology Systems were evaluated to determine if they are suitable for U.S. Geological Survey (USGS) hydrologic data collection. The sensors were evaluated in laboratory conditions to evaluate the distance accuracy of the sensor over the manufacturer’s specified operating temperatures and distance to water...
Hydrologic regime changes in a high-latitude glacierized watershed under future climate conditions
Melissa Valentin, Terri S. Hogue, Lauren Hay
2018, Water (10)
A calibrated conceptual glacio-hydrological monthly water balance model (MWBMglacier) was used to evaluate future changes in water partitioning in a high-latitude glacierized watershed in Southcentral Alaska under future climate conditions. The MWBMglacier was previously calibrated and evaluated against streamflow measurements, literature values of glacier mass balance change, and satellite-based observations...
Using a food web model to inform the design of river restoration—An example at the Barkley Bear Segment, Methow River, north-central Washington
Joseph R. Benjamin, J. Ryan Bellmore, Daniel Dombroski
2018, Open-File Report 2018-1002
With the decline of Chinook salmon (Oncorhynchus tshawytscha) and steelhead (O. mykiss), habitat restoration actions in freshwater tributaries have been implemented to improve conditions for juveniles. Typically, physical (for example, hydrologic and engineering) based models are used to design restoration alternatives with the assumption that biological responses will be improved...
Simulated hydrologic response to climate change during the 21st century in New Hampshire
David M. Bjerklie, Luke P. Sturtevant
2018, Scientific Investigations Report 2017-5143
The U.S. Geological Survey, in cooperation with the New Hampshire Department of Environmental Services and the Department of Health and Human Services, has developed a hydrologic model to assess the effects of short- and long-term climate change on hydrology in New Hampshire. This report documents the model and datasets developed...
Flood-inundation maps for the Patoka River in and near Jasper, southwestern Indiana
Kathleen K. Fowler
2018, Scientific Investigations Report 2017-5138
Digital flood-inundation maps for a 9.5-mile reach of the Patoka River in and near the city of Jasper, southwestern Indiana (Ind.), from the streamgage near County Road North 175 East, downstream to State Road 162, were created by the U.S. Geological Survey (USGS) in cooperation with the Indiana Department of...
Effects of water level and climate on the hydrodynamics and water quality of Anvil Lake, Wisconsin, a shallow seepage lake
Dale M. Robertson, Paul F. Juckem, Eric D. Dantoin, Luke A. Winslow
2018, Lake and Reservoir Management (34) 211-231
Interannual differences in the water quality of Anvil Lake, Wisconsin, were examined to determine how water level and climate affect the hydrodynamics and trophic state of shallow lakes, and their importance compared to anthropogenic changes in the watershed. Anvil Lake is a relatively pristine seepage lake with hydrology dominated by...
Development of a hydraulic model and flood-inundation maps for the Wabash River near the Interstate 64 Bridge near Grayville, Illinois
Justin A. Boldt
2018, Scientific Investigations Report 2017-5140
A two-dimensional hydraulic model and digital flood‑inundation maps were developed for a 30-mile reach of the Wabash River near the Interstate 64 Bridge near Grayville, Illinois. The flood-inundation maps, which can be accessed through the U.S. Geological Survey (USGS) Flood Inundation Mapping Science web site at http://water.usgs.gov/osw/flood_inundation/, depict...
Estimating restorable wetland water storage at landscape scales
Charles Nathan Jones, Grey R. Evenson, Daniel L. McLaughlin, Melanie K. Vanderhoof, Megan W. Lang, Greg W. McCarty, Heather E. Golden, Charles R. Lane, Laurie C. Alexander
2018, Hydrological Processes (32) 305-313
Globally, hydrologic modifications such as ditching and subsurface drainage have significantly reduced wetland water storage capacity (i.e., volume of surface water a wetland can retain) and consequent wetland functions. While wetland area has been well documented across many landscapes and used to guide restoration efforts, few studies have directly quantified...
Processing of next generation weather radar-multisensor precipitation estimates and quantitative precipitation forecast data for the DuPage County streamflow simulation system
Maitreyee Bera, Terry W. Ortel
2018, Open-File Report 2017-1159
The U.S. Geological Survey, in cooperation with DuPage County Stormwater Management Department, is testing a near real-time streamflow simulation system that assists in the management and operation of reservoirs and other flood-control structures in the Salt Creek and West Branch DuPage River drainage basins in DuPage County, Illinois. As part...
A conceptual framework for effectively anticipating water-quality changes resulting from changes in agricultural activities
Paul D. Capel, David M. Wolock, Richard H. Coupe, Jason L. Roth
2018, Scientific Investigations Report 2017-5095
Agricultural activities can affect water quality and the health of aquatic ecosystems; many water-quality issues originate with the movement of water, agricultural chemicals, and eroded soil from agricultural areas to streams and groundwater. Most agricultural activities are designed to sustain or increase crop production, while some are designed to protect...
Description of the National Hydrologic Model for use with the Precipitation-Runoff Modeling System (PRMS)
R. Steven Regan, Steven L. Markstrom, Lauren E. Hay, Roland J. Viger, Parker A. Norton, Jessica M. Driscoll, Jacob H. LaFontaine
2018, Techniques and Methods 6-B9
This report documents several components of the U.S. Geological Survey National Hydrologic Model of the conterminous United States for use with the Precipitation-Runoff Modeling System (PRMS). It provides descriptions of the (1) National Hydrologic Model, (2) Geospatial Fabric for National Hydrologic Modeling, (3) PRMS hydrologic simulation code, (4) parameters and...
Nutrient dynamics in partially drained arctic thaw lakes
Joshua C. Koch, Tom F. Fondell, Joel A. Schmutz, Sarah M. Laske
2018, Journal of Geophysical Research: Biogeosciences (123) 440-452
Thaw lakes are ubiquitous on arctic coastal plains (ACPs). While many thaw lakes have steep banks, stable water levels, and static surface areas, others only partially fill their basins and vary in area over the summer. These partially drained lakes (PDLs) are hydrologically connected to the wetlands immediately surrounding them....
Comparison of time nonlocal transport models for characterizing non-Fickian transport: From mathematical interpretation to laboratory application
Bingqing Lu, Yong Zhang, Chunmiao Zheng, Christopher T. Green, Charles O’Neill, Hong-Guang Sun, Jiazhong Qian
2018, Water (10) 1-28
Non-Fickian diffusion has been increasingly documented in hydrology and modeled by promising time nonlocal transport models. While previous studies showed that most of the time nonlocal models are identical with correlated parameters, fundamental challenges remain in real-world applications regarding model selection and parameter definition. This study compared three popular time...
High resolution water body mapping for SWAT evaporative modelling in the Upper Oconee watershed of Georgia, USA
Amber R. Ignatius, John Jones
2018, Hydrological Processes (32) 51-65
Technological improvements in remote sensing and geographic information systems have demonstrated the abundance of artificially constructed water bodies across the landscape. Although research has shown the ubiquity of small ponds globally, and in the southeastern United States in particular, their cumulative impact in terms of evaporative alteration is less well...
Advances in drainage: Selected works from the Tenth International Drainage Symposium
Jeffrey S. Strock, Christopher Hay, Matthew Helmers, Kelly A. Nelson, Gary R. Sands, R. Wayne Skaggs, Kyle R. Douglas-Mankin
2018, Transactions of the ASABE (61) 161-168
This article introduces a special collection of fourteen articles accepted from among the 140 technical presentations, posters, and meeting papers presented at the 10th International ASABE Drainage Symposium. The symposium continued in the tradition of previous symposia that began in 1965 as a forum for presenting and assessing the progress...
Managing the water-energy-food nexus: Opportunities in Central Asia
Shokhrukh Jaliliv, Saud A. Amer, Frank Ward
2018, Journal of Hydrology (557) 407-425
This article examines impacts of infrastructure development and climate variability on economic outcomes for the Amu Darya Basin in Central Asia. It aims to identify the most economically productive mix of expanded reservoir storage for economic benefit sharing to occur, in...
Drought-induced recharge promotes long-term storage of porewater salinity beneath a prairie wetland
Zeno F Levy, Donald O. Rosenberry, Robert Moucha, David M. Mushet, Martin B. Goldhaber, James W. LaBaugh, Anthony J Fiorentino, Donald I. Siegel
2018, Journal of Hydrology (557) 391-409
Subsurface storage of sulfate salts allows closed-basin wetlands in the semiarid Prairie Pothole Region (PPR) of North America to maintain moderate surface water salinity (total dissolved solids [TDS] from 1 to 10 g L−1), which provides critical habitat for communities of aquatic biota. However, it is unclear how the salinity of wetland...
Characterizing uncertainty in daily streamflow estimates at ungauged locations for the Massachusetts sustainable yield estimator
William H. Farmer, Sara B. Levin
2018, Journal of the American Water Resources Association (54) 198-210
Hydrologic characterization at ungauged locations is one of the quintessential challenges of hydrology. Beyond simulation of historical streamflows, it is similarly important to characterize the level of uncertainty in hydrologic estimates. In tandem with updates to Massachusetts Sustainable Yield Estimator, this work explores the application of...
Everglades Depth Estimation Network (EDEN)—A decade of serving hydrologic information to scientists and resource managers
Eduardo Patino, Paul Conrads, Eric D. Swain, James M. Beerens
2018, Fact Sheet 2017-3069
IntroductionThe Everglades Depth Estimation Network (EDEN) provides scientists and resource managers with regional maps of daily water levels and depths in the freshwater part of the Greater Everglades landscape. The EDEN domain includes all or parts of five Water Conservation Areas, Big Cypress National Preserve, Pennsuco Wetlands, and Everglades National...
Groundwater development stress: Global-scale indices compared to regional modeling
William Alley, Brian R. Clark, Matt Ely, Claudia C. Faunt
2018, Groundwater (56) 266-275
The increased availability of global datasets and technologies such as global hydrologic models and the Gravity Recovery and Climate Experiment (GRACE) satellites have resulted in a growing number of global-scale assessments of water availability using simple indices of water stress. Developed initially for surface water, such indices are increasingly used...
Maximizing establishment and survivorship of field-collected and greenhouse-cultivated biocrusts in a semi-cold desert
Anita Antoninka, Matthew A. Bowker, Peter Chuckran, Nicole N. Barger, Sasha C. Reed, Jayne Belnap
2018, Plant and Soil (429) 213-225
AimsBiological soil crusts (biocrusts) are soil-surface communities in drylands, dominated by cyanobacteria, mosses, and lichens. They provide key ecosystem functions by increasing soil stability and influencing soil hydrologic, nutrient, and carbon cycles. Because of this, methods to reestablish biocrusts in damaged drylands are needed. Here...