Joseph A Hevesi - California Water Science Center
Science and Products
Filter Total Items: 21
Precipitation runoff modeling system (PRMS) as part of an integrated hydrologic model for the Osage Nation, northeastern Oklahoma, 1915–2014
Executive SummaryThe Osage Nation lacks a comprehensive tribal water plan to describe the quality and quantity of water resources in the Osage Nation, a 2,304-square-mile (mi2) area of rolling pastures, tallgrass prairie, and mixed woodlands in northeastern Oklahoma. A tribal water plan can be used to help manage the sustainable development of surface and groundwater resources, thereby helping to
Authors
Joseph A. Hevesi, Randall T. Hanson, Jason R. Masoner
Integrated hydrologic modeling of the Salinas River, California, for sustainable water management
The Salinas River is the largest river in California’s Central Coast region. Groundwater resources of the Salinas River basin are used to meet water supply needs, including crop irrigation and municipal water supply. Two large multipurpose reservoirs also supply irrigation and municipal water uses. Historical imbalances between supply and demand have resulted in sinking groundwater levels, seawate
Authors
Joseph A. Hevesi, Wesley R. Henson, Randall T. Hanson, Scott E. Boyce
Estimating spatially and temporally varying recharge and runoff from precipitation and urban irrigation in the Los Angeles Basin, California
A daily precipitation-runoff model, referred to as the Los Angeles Basin watershed model (LABWM), was used to estimate recharge and runoff for a 5,047 square kilometer study area that included the greater Los Angeles area and all surface-water drainages potentially contributing recharge to a 1,450 square kilometer groundwater-study area underlying the greater Los Angeles area, referred to as the L
Authors
Joseph A. Hevesi, Tyler D. Johnson
Estimating natural recharge in San Gorgonio Pass watersheds, California, 1913–2012
A daily precipitation-runoff model was developed to estimate spatially and temporally distributed recharge for groundwater basins in the San Gorgonio Pass area, southern California. The recharge estimates are needed to define transient boundary conditions for a groundwater-flow model being developed to evaluate the effects of pumping and climate on the long-term availability of groundwater. The ar
Authors
Joseph A. Hevesi, Allen H. Christensen
Geohydrology of Big Bear Valley, California: phase 1--geologic framework, recharge, and preliminary assessment of the source and age of groundwater
The Big Bear Valley, located in the San Bernardino Mountains of southern California, has increased in population in recent years. Most of the water supply for the area is pumped from the alluvial deposits that form the Big Bear Valley groundwater basin. This study was conducted to better understand the thickness and structure of the groundwater basin in order to estimate the quantity and distribut
Authors
Lorraine E. Flint, Justin Brandt, Allen H. Christensen, Alan L. Flint, Joseph A. Hevesi, Robert Jachens, Justin T. Kulongoski, Peter Martin, Michelle Sneed
Application of a watershed model (HSPF) for evaluating sources and transport of pathogen indicators in the Chino Basin drainage area, San Bernardino County, California
A watershed model using Hydrologic Simulation Program-FORTRAN (HSPF) was developed for the urbanized Chino Basin in southern California to simulate the transport of pathogen indicator bacteria, evaluate the flow-component and land-use contributions to bacteria contamination and water-quality degradation throughout the basin, and develop a better understanding of the potential effects of climate an
Authors
Joseph A. Hevesi, Lorraine E. Flint, Clinton D. Church, Gregory O. Mendez
Decoupled application of the integrated hydrologic model, GSFLOW, to estimate agricultural irrigation in the Santa Rosa Plain, California
No abstract available.
Authors
Joseph A. Hevesi, Linda R. Woolfenden, Richard G. Niswonger, R. Steven Regan, Tracy Nishikawa
Geology, ground-water hydrology, geochemistry, and ground-water simulation of the Beaumont and Banning Storage Units, San Gorgonio Pass area, Riverside County, California
Ground water has been the only source of potable water supply for residential, industrial, and agricultural users in the Beaumont and Banning storage units of the San Gorgonio Pass area, Riverside County, California. Ground-water levels in the Beaumont area have declined as much as 100 feet between the early 1920s and early 2000s, and numerous natural springs have stopped flowing. In 1961, the San
Authors
Diane L. Rewis, Allen H. Christensen, Jonathan Matti, Joseph A. Hevesi, Tracy Nishikawa, Peter Martin
Hydrogeologic characterization of the Modesto Area, San Joaquin Valley, California
Hydrogeologic characterization was done to develop an understanding of the hydrogeologic setting near Modesto by maximizing the use of existing data and building on previous work in the region. A substantial amount of new lithologic and hydrologic data are available that allow a more complete and updated characterization of the aquifer system. In this report, geologic units are described, a databa
Authors
Karen R. Burow, Jennifer L. Shelton, Joseph A. Hevesi, Gary S. Weissmann
Fundamental concepts of recharge in the Desert Southwest: A regional modeling perspective
Recharge in arid basins does not occur in all years or at all locations within a basin. In the desert Southwest potential evapotranspiration exceeds precipitation on an average annual basis and, in many basins, on an average monthly basis. Ground-water traveltime from the surface to the water table and recharge to the water table vary temporally and spatially owing to variations in precipitation,
Authors
Alan L. Flint, Lorraine E. Flint, J.A. Hevesi
Simulation of net infiltration and potential recharge using a distributed-parameter watershed model of the Death Valley region, Nevada and California
This report presents the development and application of the distributed-parameter watershed model, INFILv3, for estimating the temporal and spatial distribution of net infiltration and potential recharge in the Death Valley region, Nevada and California. The estimates of net infiltration quantify the downward drainage of water across the lower boundary of the root zone and are used to indicate pot
Authors
Joseph A. Hevesi, Alan L. Flint, Lorraine E. Flint
Preliminary estimates of spatially distributed net infiltration and recharge for the Death Valley region, Nevada-California
A three-dimensional ground-water flow model has been developed to evaluate the Death Valley regional flow system, which includes ground water beneath the Nevada Test Site. Estimates of spatially distributed net infiltration and recharge are needed to define upper boundary conditions. This study presents a preliminary application of a conceptual and numerical model of net infiltration. The model wa
Authors
J.A. Hevesi, A. L. Flint, L. E. Flint
INFIL3.0
A Grid-Based, Distributed-Parameter Watershed Model to Estimate Net Infiltration Below the Root Zone
Science and Products
- Publications
Filter Total Items: 21
Precipitation runoff modeling system (PRMS) as part of an integrated hydrologic model for the Osage Nation, northeastern Oklahoma, 1915–2014
Executive SummaryThe Osage Nation lacks a comprehensive tribal water plan to describe the quality and quantity of water resources in the Osage Nation, a 2,304-square-mile (mi2) area of rolling pastures, tallgrass prairie, and mixed woodlands in northeastern Oklahoma. A tribal water plan can be used to help manage the sustainable development of surface and groundwater resources, thereby helping toAuthorsJoseph A. Hevesi, Randall T. Hanson, Jason R. MasonerIntegrated hydrologic modeling of the Salinas River, California, for sustainable water management
The Salinas River is the largest river in California’s Central Coast region. Groundwater resources of the Salinas River basin are used to meet water supply needs, including crop irrigation and municipal water supply. Two large multipurpose reservoirs also supply irrigation and municipal water uses. Historical imbalances between supply and demand have resulted in sinking groundwater levels, seawateAuthorsJoseph A. Hevesi, Wesley R. Henson, Randall T. Hanson, Scott E. BoyceEstimating spatially and temporally varying recharge and runoff from precipitation and urban irrigation in the Los Angeles Basin, California
A daily precipitation-runoff model, referred to as the Los Angeles Basin watershed model (LABWM), was used to estimate recharge and runoff for a 5,047 square kilometer study area that included the greater Los Angeles area and all surface-water drainages potentially contributing recharge to a 1,450 square kilometer groundwater-study area underlying the greater Los Angeles area, referred to as the LAuthorsJoseph A. Hevesi, Tyler D. JohnsonEstimating natural recharge in San Gorgonio Pass watersheds, California, 1913–2012
A daily precipitation-runoff model was developed to estimate spatially and temporally distributed recharge for groundwater basins in the San Gorgonio Pass area, southern California. The recharge estimates are needed to define transient boundary conditions for a groundwater-flow model being developed to evaluate the effects of pumping and climate on the long-term availability of groundwater. The arAuthorsJoseph A. Hevesi, Allen H. ChristensenGeohydrology of Big Bear Valley, California: phase 1--geologic framework, recharge, and preliminary assessment of the source and age of groundwater
The Big Bear Valley, located in the San Bernardino Mountains of southern California, has increased in population in recent years. Most of the water supply for the area is pumped from the alluvial deposits that form the Big Bear Valley groundwater basin. This study was conducted to better understand the thickness and structure of the groundwater basin in order to estimate the quantity and distributAuthorsLorraine E. Flint, Justin Brandt, Allen H. Christensen, Alan L. Flint, Joseph A. Hevesi, Robert Jachens, Justin T. Kulongoski, Peter Martin, Michelle SneedApplication of a watershed model (HSPF) for evaluating sources and transport of pathogen indicators in the Chino Basin drainage area, San Bernardino County, California
A watershed model using Hydrologic Simulation Program-FORTRAN (HSPF) was developed for the urbanized Chino Basin in southern California to simulate the transport of pathogen indicator bacteria, evaluate the flow-component and land-use contributions to bacteria contamination and water-quality degradation throughout the basin, and develop a better understanding of the potential effects of climate anAuthorsJoseph A. Hevesi, Lorraine E. Flint, Clinton D. Church, Gregory O. MendezDecoupled application of the integrated hydrologic model, GSFLOW, to estimate agricultural irrigation in the Santa Rosa Plain, California
No abstract available.AuthorsJoseph A. Hevesi, Linda R. Woolfenden, Richard G. Niswonger, R. Steven Regan, Tracy NishikawaGeology, ground-water hydrology, geochemistry, and ground-water simulation of the Beaumont and Banning Storage Units, San Gorgonio Pass area, Riverside County, California
Ground water has been the only source of potable water supply for residential, industrial, and agricultural users in the Beaumont and Banning storage units of the San Gorgonio Pass area, Riverside County, California. Ground-water levels in the Beaumont area have declined as much as 100 feet between the early 1920s and early 2000s, and numerous natural springs have stopped flowing. In 1961, the SanAuthorsDiane L. Rewis, Allen H. Christensen, Jonathan Matti, Joseph A. Hevesi, Tracy Nishikawa, Peter MartinHydrogeologic characterization of the Modesto Area, San Joaquin Valley, California
Hydrogeologic characterization was done to develop an understanding of the hydrogeologic setting near Modesto by maximizing the use of existing data and building on previous work in the region. A substantial amount of new lithologic and hydrologic data are available that allow a more complete and updated characterization of the aquifer system. In this report, geologic units are described, a databaAuthorsKaren R. Burow, Jennifer L. Shelton, Joseph A. Hevesi, Gary S. WeissmannFundamental concepts of recharge in the Desert Southwest: A regional modeling perspective
Recharge in arid basins does not occur in all years or at all locations within a basin. In the desert Southwest potential evapotranspiration exceeds precipitation on an average annual basis and, in many basins, on an average monthly basis. Ground-water traveltime from the surface to the water table and recharge to the water table vary temporally and spatially owing to variations in precipitation,AuthorsAlan L. Flint, Lorraine E. Flint, J.A. HevesiSimulation of net infiltration and potential recharge using a distributed-parameter watershed model of the Death Valley region, Nevada and California
This report presents the development and application of the distributed-parameter watershed model, INFILv3, for estimating the temporal and spatial distribution of net infiltration and potential recharge in the Death Valley region, Nevada and California. The estimates of net infiltration quantify the downward drainage of water across the lower boundary of the root zone and are used to indicate potAuthorsJoseph A. Hevesi, Alan L. Flint, Lorraine E. FlintPreliminary estimates of spatially distributed net infiltration and recharge for the Death Valley region, Nevada-California
A three-dimensional ground-water flow model has been developed to evaluate the Death Valley regional flow system, which includes ground water beneath the Nevada Test Site. Estimates of spatially distributed net infiltration and recharge are needed to define upper boundary conditions. This study presents a preliminary application of a conceptual and numerical model of net infiltration. The model waAuthorsJ.A. Hevesi, A. L. Flint, L. E. Flint - Software
INFIL3.0
A Grid-Based, Distributed-Parameter Watershed Model to Estimate Net Infiltration Below the Root Zone