Increasing atmospheric evaporative demand across the Tibetan plateau and implications for surface water resources.

ates the E o changes? and (3) what do E o changes imply for potential changes of surface water resources under a changing climate? Results and discussion Spatial and temporal trends in E o The time series of pan evaporation, as estimated by the PenPan model 35 (denoted E PenPan ), consistently show an increasing trend across the entire TP for 1980–2015 when using different datasets, with the exception of MERRA-2 ( Figures 1 A and 1B).

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