Geohydrology and evapotranspiration at Franklin Lake playa, Inyo County, California
Water Supply Paper
2377
By: John B. Czarnecki and David I. Stannard
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Abstract
Franklin Lake playa is one of the principal discharge areas of the ground-water-flow system associated with Yucca Mountain, Nevada, the potential site of a high-level nuclear-waste repository. By using the energy-budget eddy-correlation technique, measurements made between June 1983 and April 1984 to estimate evapotranspiration were found to range from 0.1 centimeter per day during winter months to about 0.3 centimeter per day during summer months; the annual average was 0.16 centimeter per day. These estimates were compared with evapotranspiration estimates calculated from six other methods.
Suggested Citation
Czarnecki, J.B., Stannard, D.I., 1997, Geohydrology and evapotranspiration at Franklin Lake playa, Inyo County, California: U.S. Geological Survey Water Supply Paper 2377, vi, 75 p., https://doi.org/10.3133/wsp2377.
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Geohydrology and evapotranspiration at Franklin Lake playa, Inyo County, California |
| Series title | Water Supply Paper |
| Series number | 2377 |
| DOI | 10.3133/wsp2377 |
| Year Published | 1997 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Description | vi, 75 p. |
| Country | United States |
| State | California |
| County | Inyo County |
| Other Geospatial | Franklin Lake playa |