Long-term variations in actual evapotranspiration over the Tibetan Plateau
<p>Actual terrestrial evapotranspiration (<span class="inline-formula">ET<sub>a</sub></span>) is a key parameter controlling land–atmosphere interaction processes and water cycle. However, spatial distribution and temporal changes in <span class="inlin...
Main Authors: | C. Han, Y. Ma, B. Wang, L. Zhong, W. Ma, X. Chen, Z. Su |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-07-01
|
Series: | Earth System Science Data |
Online Access: | https://essd.copernicus.org/articles/13/3513/2021/essd-13-3513-2021.pdf |
Similar Items
-
Comparison of satellite-based evapotranspiration estimates over the Tibetan
Plateau
by: J. Peng, et al.
Published: (2016-08-01) -
Combining MODIS, AVHRR and in situ data for evapotranspiration estimation over heterogeneous landscape of the Tibetan Plateau
by: Y. Ma, et al.
Published: (2014-02-01) -
Determination of land surface heat fluxes over heterogeneous landscape of the Tibetan Plateau by using the MODIS and in situ data
by: Y. Ma, et al.
Published: (2011-10-01) -
A long-term (2005–2016) dataset of hourly integrated land–atmosphere interaction observations on the Tibetan Plateau
by: Y. Ma, et al.
Published: (2020-11-01) -
Estimation of surface energy fluxes under complex terrain of Mt. Qomolangma over the Tibetan Plateau
by: X. Chen, et al.
Published: (2013-04-01)