Spatio-temporal dynamics of evapotranspiration on the Tibetan Plateau from 2000 to 2010
Submitted by susan on Tue, 2017-01-17 15:39
Evapotranspiration (ET) is a key process of the climate system because it links water, energy and carbon cycles. In this study we modified a Penman–Monteith based algorithm to estimate ET on the Tibetan Plateau at a 1 km spatial resolution for the period 2000–2010 using meteorological and satellite remote sensing data.
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11/01/2017