1 edition of Estimated ground-water discharge by evapotranspiration from Death Valley, California, 1997-2001 found in the catalog.
Estimated ground-water discharge by evapotranspiration from Death Valley, California, 1997-2001
by U.S. Dept. of the Interior, U.S. Geological Survey, U.S. Geological Survey, Information Services [distributor] in Carson City, Nev, Denver, CO
Written in English
Includes bibliographical references (p. 26-27).
|Statement||by Guy A. DeMeo ... [et al.] ; prepared in cooperation with the U.S. Department of the Interior, National Park Service and Inyo County, California.|
|Series||U.S. Geological Survey water-resources investigations report ;, 03-4254, Water-resources investigations report ;, 03-4254.|
|Contributions||DeMeo, Guy A., United States. National Park Service., Inyo County (Calif.), Geological Survey (U.S.)|
|LC Classifications||GB701 .W375 no. 03-4254|
|The Physical Object|
|Pagination||v, 27 p. :|
|Number of Pages||27|
|LC Control Number||2004356499|
Book Reviews Arthur N. Palmer & Margaret V. Palmer I assessed the influence of these environmental variables on exit counts and estimated when cave crickets emerged within the two-hour survey period. Exit-count surveys were conducted in eleven caves over four years in central Texas, and caves were surveyed up to four times a year across the. The Black Death surely ravaged the Middle East, northern Africa, and all of western and central Europe (Benedictow, ). Nevertheless the brutal pandemic did not afflict peoples in the Western Hemisphere, in sub-Saharan Africa, or in South Asia (Chaudhuri, ), although Islamic cities and regions of the eastern Mediterranean and North.
The Ground-Water Climate Response Network consists of a national network of about wells monitored as part of the USGS Ground-Water Resources Program, supplemented by more than wells monitored as part of the Cooperative Water Program that meet the . 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. Last, but assuredly not least, I express my deep gratitude to the entire McGraw-Hill book team for their enthusiasm, professionalism, and just plain hard work, without which successful completion of each subsequent edition of this book would have been impossible. Carla W. Montgomery Preface vii Page viii 1/14/
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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. Nylund. 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 wide 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.
Devitt, D. Donovan, T. 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.
From the atmosphere, rain falls on the land, and eventually finds its way back to the oceans. The volume of water on the move in this way has been estimated askm3 (cubic kilometres) a year, of whichkm3 returns to the oceans as direct precipitation andkm3 falls on land.
Precipitation Evapotranpiration Evaporation. Industrial discharge returned without treatment has high organic content, leading to rapid growth of algae, bacteria and slime, oxygen-depleted water, and thermal pollution. Discharge can affect a relatively large volume of water and have numerous impacts on human health.
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This book describes the situation of urban water management in 20 countries: all North and South American ones, and a significant number from Central America and the Caribbean region. To produce it a unique network of multidisciplinary scientists was created which in total 94 involved authors.
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