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Understanding the responses of precipitation, evaporative demand, and terrestrial water availability to planetary temperature in climate models
In many models of land hydrology, precipitation (P) and potential evapotranspiration (PET, a.k.a. evaporative demand) are the main inputs that determine actual evapotranspiration, runoff, soil moisture, and aridity or drought. In the first three chapters of this work, we attempt to understand the robust subtropical P declines, ...