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عمران::
تبخیر-تعرق
As the soil dries out, during extended periods without rain, land evapotranspiration (ET) changes from an energy-limited to a water-limited regime [Seneviratne et al.
[2010]) and soil moisture and evapotranspiration regimes (as in Seneviratne et al
Vinukollu (2015), On uncertainty in global terrestrial evapotranspiration estimates from choice of input forcing datasets, J.
Seneviratne (2014), Systematic land climate and evapotranspiration biases in CMIP5 simulations, Geophys.
(2011), Evaluation of global observations-based evapotranspiration datasets and IPCC AR4 simulations, Geophys.
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