The Long-Term Change of Latent Heat Flux over the Western Tibetan Plateau
The Tibetan Plateau (TP) has been experiencing warming and wetting since the 1980s. Under such circumstances, we estimated the summer latent heat flux (<i>LE</i>) using the maximum entropy production model driven by the net radiation, surface temperature, and soil moisture of three reana...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2020-03-01
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| Series: | Atmosphere |
| Subjects: | |
| Online Access: | https://www.mdpi.com/2073-4433/11/3/262 |