Evaluating Micrometeorological Estimates of Groundwater Discharge from Great Basin Desert Playas
Autor: | Amanda Garcia, Tracie R. Jackson, Keith J. Halford, Philip M. Gardner |
---|---|
Rok vydání: | 2018 |
Předmět: |
Hydrology
geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences 0208 environmental biotechnology Alluvial fan 02 engineering and technology Structural basin Energy budget 01 natural sciences Arid California 020801 environmental engineering Wetlands Evapotranspiration Southwestern United States Environmental science Groundwater discharge Computers in Earth Sciences Bowen ratio Groundwater Nevada 0105 earth and related environmental sciences Water Science and Technology |
Zdroj: | Groundwater. 56:909-920 |
ISSN: | 1745-6584 0017-467X |
Popis: | Groundwater availability studies in the arid southwestern United States traditionally have assumed that groundwater discharge by evapotranspiration (ETg ) from desert playas is a significant component of the groundwater budget. However, desert playa ETg rates are poorly constrained by Bowen ratio energy budget (BREB) and eddy-covariance (EC) micrometeorological measurement approaches. Best attempts by previous studies to constrain ETg from desert playas have resulted in ETg rates that are within the measurement error of micrometeorological approaches. This study uses numerical models to further constrain desert playa ETg rates that are within the measurement error of BREB and EC approaches, and to evaluate the effect of hydraulic properties and salinity-based groundwater density contrasts on desert playa ETg rates. Numerical models simulated ETg rates from desert playas in Death Valley, California and Dixie Valley, Nevada. Results indicate that actual ETg rates from desert playas are significantly below the uncertainty thresholds of BREB- and EC-based micrometeorological measurements. Discharge from desert playas likely contributes less than 2% of total groundwater discharge from Dixie and Death Valleys, which suggests discharge from desert playas also is negligible in other basins. Simulation results also show that ETg from desert playas primarily is limited by differences in hydraulic properties between alluvial fan and playa sediments and, to a lesser extent, by salinity-based groundwater density contrasts. |
Databáze: | OpenAIRE |
Externí odkaz: |