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Publications
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Precipitation in the upper Mississippi River basin, January 1 through July 31, 1993 Precipitation in the upper Mississippi River basin, January 1 through July 31, 1993
Excessive precipitation produced severe flooding in a nine-State area in the upper Mississippi River Basin during spring and summer 1993. Following a spring that was wetter than average, weather patterns that persisted from early June through July caused the upper Midwest to be deluged with an unusually large amount of rainfall. Monthly precipitation data were examined at 10 weather...
Authors
Kenneth L. Wahl, Kevin C. Vining, Gregg J. Wiche
Flood discharges in the upper Mississippi River basin, 1993 Flood discharges in the upper Mississippi River basin, 1993
From mid-June through early August 1993, flooding was severe in the upper Mississippi River Basin following a wet-weather pattern that persisted over the area for at least 6 months before the flood. The magnitude and timing of several intense rainstorms in late June and July, combined with wet antecedent climatic conditions, were the principal causes of the flooding. Flood-peak...
Authors
Charles Parrett, Nick B. Melcher, Robert W. James
Sensitivity of water resources in the Delaware River basin to climate variability and change Sensitivity of water resources in the Delaware River basin to climate variability and change
Because of the "greenhouse effect," projected increases in atmospheric carbon dioxide levels might cause global warming, which in turn could result in changes in precipitation patterns and evapotranspiration and in increases in sea level. This report describes the greenhouse effect; discusses the problems and uncertainties associated with the detection, prediction, and effects of...
Authors
Mark A. Ayers, David M. Wolock, Gregory J. McCabe, Lauren E. Hay, Gary D. Tasker
National water summary 1990-91: Hydrologic events and stream water quality National water summary 1990-91: Hydrologic events and stream water quality
National Water Summary 1990-91 Hydrologic Events and Stream Water Quality was planned to complement existing Federal-State water-quality reporting to the U.S. Congress that is required by the Clean Water Act of 1972. This act, formally known as the Federal Water Pollution Control Act Amendments of 1972 (Public Law 92-500), and its amendments in 1977,1979,1980,1981,1983, and 1987, is the...
Geohydrologic systems in Kansas — Geohydrology of the lower aquifer unit in the western interior plains aquifer system Geohydrologic systems in Kansas — Geohydrology of the lower aquifer unit in the western interior plains aquifer system
No abstract available.
Authors
L. J. Combs, Cristi V. Hansen, R. J. Wolf
Geohydrologic systems in Kansas — Geohydrology of the lower aquifer unit in the western interior plains aquifer system Geohydrologic systems in Kansas — Geohydrology of the lower aquifer unit in the western interior plains aquifer system
The purpose of the investigation is to provide a description of the principal geohydrologic systems in Upper Cambrian through Lower Cretaceous rocks in Kansas. This investigation was made as part of the Central Midwest Regional Aquifer-System Analysis (CMRASA). The CMRASA is one of several major investigations by the U.S. Geological Survey of regional aquifer systems in the United States...
Authors
J. F. Kenny, Cristi V. Hansen, R. J. Wolf
Hydrology of the Great Plains aquifer system in Nebraska, Colorado, Kansas, and adjacent areas Hydrology of the Great Plains aquifer system in Nebraska, Colorado, Kansas, and adjacent areas
No abstract available.
Authors
J. O. Helgesen, R. B. Leonard, R. J. Wolf
Regional aquifers in Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: Geohydrologic framework Regional aquifers in Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: Geohydrologic framework
Regional aquifers are described within a 370,000-square-mile area extending from the foothills of the Rocky Mountains in Colorado to the Missouri and Mississippi Rivers in eastern Nebraska and Missouri, and from South Dakota to the Ouachita, Arbuckle, and Wichita Mountains of Arkansas and Oklahoma. The present geohydrologic framework of aquifers and confining units in this area is...
Authors
Donald G. Jorgensen, John O. Helgesen, Jeffrey L. Imes
Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL Simulating the variable-source-area concept of streamflow generation with the watershed model TOPMODEL
This report describes TOPMODEL, which is a physically based watershed model that simulates the variable-source-area concept of streamflow generation. The report describes the theoretical background, model equations, methods to determine parameter values, Fortran computer code, and an example interactive simulation. Using TOPMODEL requires specification of soils and topographic parameters
Authors
D.M. Wolock
Ground- and surface-water interaction between the Kansas River and associated alluvial aquifer, northeastern Kansas Ground- and surface-water interaction between the Kansas River and associated alluvial aquifer, northeastern Kansas
No abstract available.
Authors
R. J. Wolf, J. O. Helgesen
Description of water-resource-related data compiled for Reno County, south-central Kansas Description of water-resource-related data compiled for Reno County, south-central Kansas
Water-resource-related data for sites in Reno County, Kansas were compiled in cooperation with the Reno County Health Department as part of the Kansas Department of Health and Environment's Local Environmental Protection Program (LEPP). These data were entered into a relational data-base management system (RDBMS) to facilitate the spatial analysis required to meet the LEPP goals of...
Authors
C. V. Hansen
The occurrence and transport of agricultural pesticides in the Tuttle Creek lake-stream system, Kansas and Nebraska The occurrence and transport of agricultural pesticides in the Tuttle Creek lake-stream system, Kansas and Nebraska
No abstract available.
Authors
H.E. Bevans, C. H. Fromm, S.A. Watkins