Estimated ground-water discharge by evapotranspiration from Death Valley, California, 1997-2001

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U.S. Geological Survey, U.S. Geological Survey Information Services [distributor] , Carson City, Nev, Denver, CO
Evapotranspiration -- Death Valley (Calif. and Nev.), Groundwater flow -- Death Valley (Calif. and
Other titlesEstimated ground water discharge by evapotranspiration from Death Valley, California, 1997-2001
Statementby Guy A. DeMeo ... [et al.] ; prepared in cooperation with the U.S. Department of the Interior, National Park Service and Inyo County, California
SeriesWater-resources investigations report -- 03-4254
ContributionsDeMeo, Guy A., Inyo County (Calif.), United States. National Park Service, Geological Survey (U.S.)
The Physical Object
Paginationv, 27 p. :
ID Numbers
Open LibraryOL18154229M

The total ground-water discharge from ET for the Death Valley floor is ab acre-feet and was computed by summ ing the products of the area of each ET unit mul tiplied by a corresponding ET rate for each unit. Estimated Ground-Water Discharge by Evapotranspiration from Death Valley, California, – Estimated ground-water discharge by evapotranspiration from Death Valley, California, Water-Resources Investigations Report Estimated Ground-Water Discharge by Evapotranspiration from Death Valley, California, By Guy A.

DeMeo, Randell J. Laczniak, Robert A. Boyd, J. LaRue Smith, and Walter E.

Details Estimated ground-water discharge by evapotranspiration from Death Valley, California, 1997-2001 PDF

Estimated ground-water discharge by evapotranspiration from Death Valley. Report availability: Portable Document Format (PDF). Abstract. Estimated ground-water discharge by evapotranspiration from Death Valley, California, / (Carson City, Nev.: U.S.

Geological Survey ; Regional ground-water evapotranspiration and ground- water budgets, Great Basin, Nevada / (Reston. Estimated Ground-water Discharge by Evapotranspiration from Death Valley, California, – US Geological Survey Water-Resources Investigation Reportpp.

Google Scholar Fetter, Cited by: Estimating groundwater recharge in arid or semiarid regions can be a difficult and complex task, since it is dependent on a highly variable set of spatial and temporal hydrologic parameters and processes that are dependent on the local climate, the land surface properties, and subsurface characteristics.

As a result, traditional methods for estimating the recharge can result in a California Cited by: 2. Estimated ground-water discharge by evapotranspiration from Death Valley, California, – US Geological Survey Water-Resources Investigation Report 03 Cited by: Estimated ground-water discharge by evapotranspiration from Death Valley, California, GBW no Historical ground-water-flow patterns and trends in iron concentrations in the Potomac--Raritan--Magothy aquifer system in parts of Philadelphia, Pennsylvania, and Camden and Gloucester Counties, New Jersey.

Location of Death Valley Regional Ground-Water Flow System and the Nevada Test Site. Calculating Evapotranspiration for Rainier Mesa, W.E.,Estimated ground-water discharge. Journal of the American Watre Resouirces Association A reevaluation of the ground water budget for Las Vegas Valley, Nevada, with Emphasis on ground water discharge, by D.

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Katzer, and M. Johnson, reprint from Journal of the American Watre Resouirces Association, vol. 38, no. 6, Decemberp. Figure 7. Southern subbasins of Amargosa River drainage basin with topographically enhanced satellite image as a base. The Tecopa (Tc) and the southern Death Valley (SDV) subbasins are shown along the main stem channel of the Amargosa River, and the California Valley (CV) and the Salt Creek (SC) subbasins are shown along major tributaries.

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Description Estimated ground-water discharge by evapotranspiration from Death Valley, California, 1997-2001 EPUB

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水文地质工程地质, [ 3 ] DeMeo G A,Laczniak R J,Boyd R A,et al. Estimated Ground-Water Discharge by Evapotranspiration from Death Investigations Report , Valley, California, ~[R].Read: In the high hills in the central part rainfall (some 1,–1, mm, as estimated on ecological grounds) exceeds evapotranspiration for a period of about two months, and in combination with.

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Carla W. Montgomery Preface vii Page viii 1/14/  Ground-water, surface-water, and water-chemistry data, Black Mesa area, Northeastern Arizona: USGS Publications Warehouse.

Thomas, Blakemore E.; Truini, Margot. to at Polacca Wash. Median flows for November, December, January, and February of each water year are used as an index of ground-water discharge to .THE WHAT: EARTH OBSERVATION FOR WATER RESOURCES MANAGEMENT Some key variables are usually involved in these activities and, given the present state-ofthe-art technology, may be estimated using.