Brian A. Ebel
Brian Ebel is a Research Hydrologist for the USGS Water Resources Mission Area.
Brian Ebel is a hydrologist who uses field measurements combined with numerical modeling to advance prediction and assessment for water resources through improved process representation. His work focuses on landscape disturbance impacts (e.g., wildfire, forestry, legacy mining) on water availability and water-related hazards to human lives and infrastructure. He was awarded the Presidential Early Career Award for Scientists and Engineers (PECASE) in 2019 for his contributions to understanding post-wildfire flooding and water availability issues. In 2023, Brian was selected as a Kavli Fellow by the National Academy of Sciences. Brian is currently in the Earth System Processes Division of the USGS Water Resources Mission Area.
Professional Experience
2014-present: Research Hydrologist, U.S. Geological Survey, Water Mission Area
2013-2014: Research Assistant Professor, Colorado School of Mines
2012-2013: Research Assistant Professor, University of Colorado-Boulder
2008-2012: Hydrologist, U.S. Geological Survey, Water Resources Mission Area
Education and Certifications
Stanford University, Ph.D. in Hydrogeology
Washington University in St. Louis, B.A. in Earth and Planetary Science
Science and Products
Filter Total Items: 14
No Result Found
Filter Total Items: 63
Temporal evolution of measured and simulated infiltration following wildfire in the Colorado Front Range, USA: Shifting thresholds of runoff generation and hydrologic hazards Temporal evolution of measured and simulated infiltration following wildfire in the Colorado Front Range, USA: Shifting thresholds of runoff generation and hydrologic hazards
Destructive flash floods and debris flows are a common menace following wildfire. The restoration of protection provided by forests from post-fire floods and debris flows depends on the recovery of infiltration and attendant reduction of infiltration-excess surface runoff generation. This work examines seven years of post-fire infiltration measurements and temporal relations fit to soil...
Authors
Brian A. Ebel
Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings
The destructive and deadly nature of debris flows has motivated research into empirical rainfall thresholds to provide situational awareness, inform early warning systems, and reduce loss of life and property. Disturbances such as wildfire and land-cover change can influence the hydrological processes of infiltration and runoff generation; in steep terrain this typically lowers empirical
Authors
Benjamin B. Mirus, Dennis M. Staley, Jason W. Kean, Joel B. Smith, Rick Wooten, Luke A. McGuire, Brian A. Ebel
Measurement method has a larger impact than spatial scale for plot-scale field-saturated hydraulic conductivity (Kfs) after wildfire and prescribed fire in forests Measurement method has a larger impact than spatial scale for plot-scale field-saturated hydraulic conductivity (Kfs) after wildfire and prescribed fire in forests
Abstract Wildfires raise risks of floods, debris flows, major geomorphologic and sedimentologic change, and water quality and quantity shifts. A principal control on the magnitude of these changes is field-saturated hydraulic conductivity (Kfs), which dictates surface runoff generation and is a key input into numerical models. This work synthesizes 73 Kfs datasets from the literature in...
Authors
Brian Ebel
Sources of inherent infiltration variability in postwildfire soils Sources of inherent infiltration variability in postwildfire soils
An automated disc infiltrometer was developed to improve the measurements of soil hydraulic properties (saturated hydraulic conductivity and sorptivity) of soils affected by wildfire. Guidelines are given for interpreting curves showing cumulative infiltration as a function of time measured by the autodisc. The autodisc was used to measure the variability of these soil hydraulic...
Authors
John A. Moody, Richard G. Martin, Brian A. Ebel
Soil physical, hydraulic, and thermal properties in interior Alaska, USA: Implications for hydrologic response to thawing permafrost conditions Soil physical, hydraulic, and thermal properties in interior Alaska, USA: Implications for hydrologic response to thawing permafrost conditions
Boreal forest regions are a focal point for investigations of coupled water and biogeochemical fluxes in response to wildfire disturbances, climate warming, and permafrost thaw. Soil hydraulic, physical, and thermal property measurements for mineral soils in permafrost regions are limited, despite substantial influences on cryohydrogeologic model results. This work expands mineral soil...
Authors
Brian A. Ebel, Joshua C. Koch, Michelle A. Walvoord
Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon
Permafrost thaw alters subsurface flow in boreal regions that in turn influences the magnitude, seasonality, and chemical composition of streamflow. Prediction of these changes is challenged by incomplete knowledge of timing, flowpath depth, and amount of groundwater discharge to streams in response to thaw. One important phenomenon that may affect flow and transport through boreal...
Authors
Michelle A. Walvoord, Clifford I. Voss, Brian A. Ebel, Burke J. Minsley
Multi-scale geophysical mapping of deep permafrost change after disturbance in interior Alaska, USA Multi-scale geophysical mapping of deep permafrost change after disturbance in interior Alaska, USA
Disturbance related to fire or hydrologic processes can cause degradation of deep (greater than 1 m) permafrost. These changes in deep permafrost have the potential to impact landscapes and infrastructure, alter the routing and distribution of surface water or groundwater, and may contribute to the flux of carbon to terrestrial and aquatic ecosystems. However, characterization of deep...
Authors
Burke J. Minsley, Benjamin R. Bloss, Brian A. Ebel, David Matthew Rey, Michelle A. Walvoord, Dana R.N. Brown, Ronald Daanen, Abraham M. Emond, M. Andy Kass, Neal J. Pastick, Bruce Wylie
Thresholds and relations for soil‐hydraulic and soil‐physical properties as a function of burn severity 4 years after the 2011 Las Conchas Fire, New Mexico, USA Thresholds and relations for soil‐hydraulic and soil‐physical properties as a function of burn severity 4 years after the 2011 Las Conchas Fire, New Mexico, USA
Wildfire effects on soil‐physical and ‐hydraulic properties as a function of burn severity are poorly characterized, especially several years after wildfire. A stratified random sampling approach was used in 2015 to sample seven sites representing a spectrum of remotely sensed burn severity in the area impacted by the 2011 Las Conchas Fire in New Mexico, USA. Replicate samples from each...
Authors
Brian A. Ebel, Orlando C. Romero, Deborah A. Martin
Field and laboratory hydraulic characterization of landslide-prone soils in the Oregon Coast Range and implications for hydrologic simulation Field and laboratory hydraulic characterization of landslide-prone soils in the Oregon Coast Range and implications for hydrologic simulation
Unsaturated zone flow processes are an important focus of landslide hazard estimation. Differences in soil hydraulic behavior between wetting and drying conditions (i.e., hydraulic hysteresis) may be important in landslide triggering. Hydraulic hysteresis can complicate soil hydraulic parameter estimates and impact prediction capability. This investigation focused on hydraulic property...
Authors
Brian A. Ebel, Jonathan W. Godt, Ning Lu, Jeffrey A. Coe, Joel B. Smith, Rex L. Baum
Fire, flood, and drought: Extreme climate events alter flow paths and stream chemistry Fire, flood, and drought: Extreme climate events alter flow paths and stream chemistry
Extreme climate events—such as hurricanes, droughts, extreme precipitation, and wildfires—have the potential to alter watershed processes and stream response. Yet due to the destructive and hazardous nature and unpredictability of such events, capturing their hydrochemical signal is challenging. A 5‐year postwildfire study of stream chemistry in the Fourmile Creek watershed, Colorado...
Authors
Sheila F. Murphy, R. Blaine McCleskey, Deborah A. Martin, Jeffrey H. Writer, Brian A. Ebel
Postwildfire measurement of soil physical and hydraulic properties at selected sampling sites in the 2011 Las Conchas wildfire burn scar, Jemez Mountains, north-central New Mexico Postwildfire measurement of soil physical and hydraulic properties at selected sampling sites in the 2011 Las Conchas wildfire burn scar, Jemez Mountains, north-central New Mexico
The generation of runoff and the resultant flash flooding can be substantially larger following wildfire than for similar rainstorms that precede wildfire disturbance. Flash flooding after the 2011 Las Conchas Fire in New Mexico provided the motivation for this investigation to assess postwildfire effects on soil-hydraulic properties (SHPs) and soil-physical properties (SPPs) as a...
Authors
Orlando C. Romero, Brian A. Ebel, Deborah A. Martin, Katie W. Buchan, Alanna D. Jornigan
The evolution of a colluvial hollow to a fluvial channel with periodic steps following two transformational disturbances: A wildfire and a historic flood The evolution of a colluvial hollow to a fluvial channel with periodic steps following two transformational disturbances: A wildfire and a historic flood
The transition of a colluvial hollow to a fluvial channel with discrete steps was observed after two landscape-scale disturbances. The first disturbance, a high-severity wildfire, changed the catchment hydrology to favor overland flow, which incised a colluvial hollow, creating a channel in the same location. This incised channel became armored with cobbles and boulders following...
Authors
Francis K. Rengers, Luke McGuire, Brian A. Ebel, G. E. Tucker
Non-USGS Publications**
Ebel, B. A., 2013, Simulated unsaturated flow processes after wildfire and interactions with slope aspect, Water Resources Research, 49, 8090–8107, doi: 10.1002/2013WR014129
Loague, K., and , B. A. Ebel, 2013, Conceptualization in catchment modeling. In Treatise on Geomorphology, Edited by J. F. Shroder, Vol. 7, pp. 105-121. San Diego, Academic Press, doi: 10.1016/B978-0-12-374739-6.00154-8
Ebel, B. A., K. Loague, and R. I. Borja, 2010, The impacts of hysteresis on variably-saturated hydrologic response and slope failure, Environmental Earth Sciences, 61, 1215-1225, doi: 10.1007/s12665-009-0445-2
BeVille, S. H., B. B. Mirus, B. A. Ebel, G. G. Mader, and K. Loague, 2010, Using simulated hydrologic response to revisit the 1973 Lerida Court landslide, Environmental Earth Sciences, 61, 1249-1257, doi: 10.1007/s12665-010-0448-z
Ebel, B. A., K. Loague, D. R. Montgomery, and W. E. Dietrich, 2008, Physics-based continuous simulation of long-term near-surface hydrologic response for the Coos Bay experimental catchment, Water Resources Research, 44, W07417, doi:10.1029/2007WR006442
Ebel, B. A., and K. Loague, 2008, Rapid simulated hydrologic response within the variably saturated near surface, Hydrological Processes, 22, 464-471, doi:10.1002/hyp.6926
Ebel, B. A., K. Loague, W. E. Dietrich, D. R. Montgomery, R. Torres, S. P. Anderson, and T. W. Giambelluca, 2007, Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 1. Sprinkling experiments, American Journal of Science, 307, 678-708, doi:10.2475/04.2007.02
Ebel, B. A., K. Loague, J. E. VanderKwaak, W. E. Dietrich, D. R. Montgomery, R. Torres, and S. P. Anderson, 2007, Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 2. Physics-based simulations, American Journal of Science, 307, 709-748, doi:10.2475/04.2007.03
Mirus, B. B., B. A. Ebel, K. Loague, and B. C. Wemple, 2007, Simulated effect of a forest road on near-surface hydrologic response: Redux, Earth Surface Processes and Landforms, 32, 126–142, doi: 10.1002/esp.1387
Ebel, B. A., and K. Loague, 2006, Physics-based hydrologic-response simulation: Seeing through the fog of equifinality, Hydrological Processes, 20, 2887–2900, doi:10.1002/hyp.6388
Borja, R. I., G. Oettl, B. Ebel, and K. Loague, 2006, Hydrologically driven slope failure initiation in variably saturated porous media. In Modern Trends in Geomechanics. Wu, W. and H.S. Yu (Eds.), pp. 303-311, Springer-Verlag, Berlin Heidelberg, doi: 10.1007/978-3-540-35724-7_18
Loague, K., C. S. Heppner, B. B. Mirus, B. A. Ebel, Q. Ran, A. E. Carr, S. H. BeVille, and J. E. Vander Kwaak, 2006, Physics-based hydrologic-response simulation: foundation for hydroecology and hydrogeomorphology, Hydrological Processes, 20, 1231–1237, doi:10.1002/hyp.6388
Ehlmann, B. L., R. E. Arvidson, B. L. Jolliff, S. S. Johnson, B. Ebel, N. Lovenduski, J. D. Morris, J. A. Byers, N. O. Snider, and R. E. Criss, 2005, Hydrologic and Isotopic Modeling of Alpine Lake Waiau, Mauna Kea, Hawai‘i, Pacific Science, 59, 1–15, doi:10.1353/psc.2005.0005
Loague, K., C. S. Heppner, R. H. Abrams, A. E. Carr, J. E. VanderKwaak, and B. A. Ebel, 2005, Further testing of the Integrated Hydrology Model (InHM): event-based simulations for a small rangeland catchment located near Chickasha, Oklahoma, Hydrological Processes, 19, 1373–1398, doi:10.1002/hyp.5566
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 14
No Result Found
Filter Total Items: 63
Temporal evolution of measured and simulated infiltration following wildfire in the Colorado Front Range, USA: Shifting thresholds of runoff generation and hydrologic hazards Temporal evolution of measured and simulated infiltration following wildfire in the Colorado Front Range, USA: Shifting thresholds of runoff generation and hydrologic hazards
Destructive flash floods and debris flows are a common menace following wildfire. The restoration of protection provided by forests from post-fire floods and debris flows depends on the recovery of infiltration and attendant reduction of infiltration-excess surface runoff generation. This work examines seven years of post-fire infiltration measurements and temporal relations fit to soil...
Authors
Brian A. Ebel
Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings Conceptual framework for assessing disturbance impacts on debris-flow initiation thresholds across hydroclimatic settings
The destructive and deadly nature of debris flows has motivated research into empirical rainfall thresholds to provide situational awareness, inform early warning systems, and reduce loss of life and property. Disturbances such as wildfire and land-cover change can influence the hydrological processes of infiltration and runoff generation; in steep terrain this typically lowers empirical
Authors
Benjamin B. Mirus, Dennis M. Staley, Jason W. Kean, Joel B. Smith, Rick Wooten, Luke A. McGuire, Brian A. Ebel
Measurement method has a larger impact than spatial scale for plot-scale field-saturated hydraulic conductivity (Kfs) after wildfire and prescribed fire in forests Measurement method has a larger impact than spatial scale for plot-scale field-saturated hydraulic conductivity (Kfs) after wildfire and prescribed fire in forests
Abstract Wildfires raise risks of floods, debris flows, major geomorphologic and sedimentologic change, and water quality and quantity shifts. A principal control on the magnitude of these changes is field-saturated hydraulic conductivity (Kfs), which dictates surface runoff generation and is a key input into numerical models. This work synthesizes 73 Kfs datasets from the literature in...
Authors
Brian Ebel
Sources of inherent infiltration variability in postwildfire soils Sources of inherent infiltration variability in postwildfire soils
An automated disc infiltrometer was developed to improve the measurements of soil hydraulic properties (saturated hydraulic conductivity and sorptivity) of soils affected by wildfire. Guidelines are given for interpreting curves showing cumulative infiltration as a function of time measured by the autodisc. The autodisc was used to measure the variability of these soil hydraulic...
Authors
John A. Moody, Richard G. Martin, Brian A. Ebel
Soil physical, hydraulic, and thermal properties in interior Alaska, USA: Implications for hydrologic response to thawing permafrost conditions Soil physical, hydraulic, and thermal properties in interior Alaska, USA: Implications for hydrologic response to thawing permafrost conditions
Boreal forest regions are a focal point for investigations of coupled water and biogeochemical fluxes in response to wildfire disturbances, climate warming, and permafrost thaw. Soil hydraulic, physical, and thermal property measurements for mineral soils in permafrost regions are limited, despite substantial influences on cryohydrogeologic model results. This work expands mineral soil...
Authors
Brian A. Ebel, Joshua C. Koch, Michelle A. Walvoord
Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon
Permafrost thaw alters subsurface flow in boreal regions that in turn influences the magnitude, seasonality, and chemical composition of streamflow. Prediction of these changes is challenged by incomplete knowledge of timing, flowpath depth, and amount of groundwater discharge to streams in response to thaw. One important phenomenon that may affect flow and transport through boreal...
Authors
Michelle A. Walvoord, Clifford I. Voss, Brian A. Ebel, Burke J. Minsley
Multi-scale geophysical mapping of deep permafrost change after disturbance in interior Alaska, USA Multi-scale geophysical mapping of deep permafrost change after disturbance in interior Alaska, USA
Disturbance related to fire or hydrologic processes can cause degradation of deep (greater than 1 m) permafrost. These changes in deep permafrost have the potential to impact landscapes and infrastructure, alter the routing and distribution of surface water or groundwater, and may contribute to the flux of carbon to terrestrial and aquatic ecosystems. However, characterization of deep...
Authors
Burke J. Minsley, Benjamin R. Bloss, Brian A. Ebel, David Matthew Rey, Michelle A. Walvoord, Dana R.N. Brown, Ronald Daanen, Abraham M. Emond, M. Andy Kass, Neal J. Pastick, Bruce Wylie
Thresholds and relations for soil‐hydraulic and soil‐physical properties as a function of burn severity 4 years after the 2011 Las Conchas Fire, New Mexico, USA Thresholds and relations for soil‐hydraulic and soil‐physical properties as a function of burn severity 4 years after the 2011 Las Conchas Fire, New Mexico, USA
Wildfire effects on soil‐physical and ‐hydraulic properties as a function of burn severity are poorly characterized, especially several years after wildfire. A stratified random sampling approach was used in 2015 to sample seven sites representing a spectrum of remotely sensed burn severity in the area impacted by the 2011 Las Conchas Fire in New Mexico, USA. Replicate samples from each...
Authors
Brian A. Ebel, Orlando C. Romero, Deborah A. Martin
Field and laboratory hydraulic characterization of landslide-prone soils in the Oregon Coast Range and implications for hydrologic simulation Field and laboratory hydraulic characterization of landslide-prone soils in the Oregon Coast Range and implications for hydrologic simulation
Unsaturated zone flow processes are an important focus of landslide hazard estimation. Differences in soil hydraulic behavior between wetting and drying conditions (i.e., hydraulic hysteresis) may be important in landslide triggering. Hydraulic hysteresis can complicate soil hydraulic parameter estimates and impact prediction capability. This investigation focused on hydraulic property...
Authors
Brian A. Ebel, Jonathan W. Godt, Ning Lu, Jeffrey A. Coe, Joel B. Smith, Rex L. Baum
Fire, flood, and drought: Extreme climate events alter flow paths and stream chemistry Fire, flood, and drought: Extreme climate events alter flow paths and stream chemistry
Extreme climate events—such as hurricanes, droughts, extreme precipitation, and wildfires—have the potential to alter watershed processes and stream response. Yet due to the destructive and hazardous nature and unpredictability of such events, capturing their hydrochemical signal is challenging. A 5‐year postwildfire study of stream chemistry in the Fourmile Creek watershed, Colorado...
Authors
Sheila F. Murphy, R. Blaine McCleskey, Deborah A. Martin, Jeffrey H. Writer, Brian A. Ebel
Postwildfire measurement of soil physical and hydraulic properties at selected sampling sites in the 2011 Las Conchas wildfire burn scar, Jemez Mountains, north-central New Mexico Postwildfire measurement of soil physical and hydraulic properties at selected sampling sites in the 2011 Las Conchas wildfire burn scar, Jemez Mountains, north-central New Mexico
The generation of runoff and the resultant flash flooding can be substantially larger following wildfire than for similar rainstorms that precede wildfire disturbance. Flash flooding after the 2011 Las Conchas Fire in New Mexico provided the motivation for this investigation to assess postwildfire effects on soil-hydraulic properties (SHPs) and soil-physical properties (SPPs) as a...
Authors
Orlando C. Romero, Brian A. Ebel, Deborah A. Martin, Katie W. Buchan, Alanna D. Jornigan
The evolution of a colluvial hollow to a fluvial channel with periodic steps following two transformational disturbances: A wildfire and a historic flood The evolution of a colluvial hollow to a fluvial channel with periodic steps following two transformational disturbances: A wildfire and a historic flood
The transition of a colluvial hollow to a fluvial channel with discrete steps was observed after two landscape-scale disturbances. The first disturbance, a high-severity wildfire, changed the catchment hydrology to favor overland flow, which incised a colluvial hollow, creating a channel in the same location. This incised channel became armored with cobbles and boulders following...
Authors
Francis K. Rengers, Luke McGuire, Brian A. Ebel, G. E. Tucker
Non-USGS Publications**
Ebel, B. A., 2013, Simulated unsaturated flow processes after wildfire and interactions with slope aspect, Water Resources Research, 49, 8090–8107, doi: 10.1002/2013WR014129
Loague, K., and , B. A. Ebel, 2013, Conceptualization in catchment modeling. In Treatise on Geomorphology, Edited by J. F. Shroder, Vol. 7, pp. 105-121. San Diego, Academic Press, doi: 10.1016/B978-0-12-374739-6.00154-8
Ebel, B. A., K. Loague, and R. I. Borja, 2010, The impacts of hysteresis on variably-saturated hydrologic response and slope failure, Environmental Earth Sciences, 61, 1215-1225, doi: 10.1007/s12665-009-0445-2
BeVille, S. H., B. B. Mirus, B. A. Ebel, G. G. Mader, and K. Loague, 2010, Using simulated hydrologic response to revisit the 1973 Lerida Court landslide, Environmental Earth Sciences, 61, 1249-1257, doi: 10.1007/s12665-010-0448-z
Ebel, B. A., K. Loague, D. R. Montgomery, and W. E. Dietrich, 2008, Physics-based continuous simulation of long-term near-surface hydrologic response for the Coos Bay experimental catchment, Water Resources Research, 44, W07417, doi:10.1029/2007WR006442
Ebel, B. A., and K. Loague, 2008, Rapid simulated hydrologic response within the variably saturated near surface, Hydrological Processes, 22, 464-471, doi:10.1002/hyp.6926
Ebel, B. A., K. Loague, W. E. Dietrich, D. R. Montgomery, R. Torres, S. P. Anderson, and T. W. Giambelluca, 2007, Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 1. Sprinkling experiments, American Journal of Science, 307, 678-708, doi:10.2475/04.2007.02
Ebel, B. A., K. Loague, J. E. VanderKwaak, W. E. Dietrich, D. R. Montgomery, R. Torres, and S. P. Anderson, 2007, Near-surface hydrologic response for a steep, unchanneled catchment near Coos Bay, Oregon: 2. Physics-based simulations, American Journal of Science, 307, 709-748, doi:10.2475/04.2007.03
Mirus, B. B., B. A. Ebel, K. Loague, and B. C. Wemple, 2007, Simulated effect of a forest road on near-surface hydrologic response: Redux, Earth Surface Processes and Landforms, 32, 126–142, doi: 10.1002/esp.1387
Ebel, B. A., and K. Loague, 2006, Physics-based hydrologic-response simulation: Seeing through the fog of equifinality, Hydrological Processes, 20, 2887–2900, doi:10.1002/hyp.6388
Borja, R. I., G. Oettl, B. Ebel, and K. Loague, 2006, Hydrologically driven slope failure initiation in variably saturated porous media. In Modern Trends in Geomechanics. Wu, W. and H.S. Yu (Eds.), pp. 303-311, Springer-Verlag, Berlin Heidelberg, doi: 10.1007/978-3-540-35724-7_18
Loague, K., C. S. Heppner, B. B. Mirus, B. A. Ebel, Q. Ran, A. E. Carr, S. H. BeVille, and J. E. Vander Kwaak, 2006, Physics-based hydrologic-response simulation: foundation for hydroecology and hydrogeomorphology, Hydrological Processes, 20, 1231–1237, doi:10.1002/hyp.6388
Ehlmann, B. L., R. E. Arvidson, B. L. Jolliff, S. S. Johnson, B. Ebel, N. Lovenduski, J. D. Morris, J. A. Byers, N. O. Snider, and R. E. Criss, 2005, Hydrologic and Isotopic Modeling of Alpine Lake Waiau, Mauna Kea, Hawai‘i, Pacific Science, 59, 1–15, doi:10.1353/psc.2005.0005
Loague, K., C. S. Heppner, R. H. Abrams, A. E. Carr, J. E. VanderKwaak, and B. A. Ebel, 2005, Further testing of the Integrated Hydrology Model (InHM): event-based simulations for a small rangeland catchment located near Chickasha, Oklahoma, Hydrological Processes, 19, 1373–1398, doi:10.1002/hyp.5566
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.