HYDROLOGY AND SURFACE ENERGY BUDGET AT THE SALAR DE ATACAMA, CHILE
In this talk, we present an overview of the hydrology of the Salar de Atacama and focus on the largest sink of water in the basin; evaporation from the salar surface. Quantification of the seasonal rates of evaporation are critical to development of water budget projections for the salar and to provide proper management of both mineral and ecosystem resources. While previous work has shown that evaporation from playas is controlled by both the depth to the saturated zone and the surface soils and/or salt crust, evaporation estimates are often based on very local scale measurements. These local scale measurements must then be up-scaled 6-7 orders of magnitude to encompass the large area of the discharging salar. To integrate at larger scales, field measurements of surface energy balance and CO2 flux are planned for the Chilean winter using eddy covariance methods capable of integrating evaporative flux over km-scale regions. These measurements, combined with remote sensing of the salar surface will be used to infer salar-scale estimates of seasonal evaporation and biogeochemical processes from this remote and hyper-arid region.