Articles | Volume 29, issue 2
https://doi.org/10.5194/hess-29-485-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-29-485-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
How much water vapour does the Tibetan Plateau release into the atmosphere?
Key Laboratory of Remote Sensing and Digital Earth, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100101, China
Li Jia
Key Laboratory of Remote Sensing and Digital Earth, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100101, China
Guangcheng Hu
Key Laboratory of Remote Sensing and Digital Earth, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100101, China
Massimo Menenti
Key Laboratory of Remote Sensing and Digital Earth, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100101, China
Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, the Netherlands
Joris Timmermans
Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, the Netherlands
Related authors
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Mahmoud H. Ahmed, Roderik Lindenbergh, Massimo Menenti, and Joris Timmermans
ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci., XI-3-2026, 695–704, https://doi.org/10.5194/isprs-annals-XI-3-2026-695-2026, https://doi.org/10.5194/isprs-annals-XI-3-2026-695-2026, 2026
Wen Wen, Joris Timmermans, Qi Chen, and Peter M. van Bodegom
Hydrol. Earth Syst. Sci., 26, 4537–4552, https://doi.org/10.5194/hess-26-4537-2022, https://doi.org/10.5194/hess-26-4537-2022, 2022
Short summary
Short summary
A novel approach for evaluating individual and combined impacts of drought and salinity in real-life settings is proposed using Sentinel-2. We found that crop responses to drought and salinity differ between growth stages. Compared to salinity, crop growth is most strongly affected by drought stress and is, in general, further exacerbated when co-occurring with salinity stress. Our approach facilitates a way to monitor crop health under multiple stresses with potential large-scale applications.
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Short summary
Reliable quantification of the amount and variability of evapotranspiration (ET) on the Tibetan Plateau is important for understanding the regional water cycle and resources. This study compares 22 ET products and finds that the mean annual ET over the Tibetan Plateau is 333.1 mm yr-1, and most products show an increasing trend. It also finds that soil evaporation is the largest contributor to total ET and that contributions from open-water evaporation and snow/ice sublimation cannot be ignored.
Reliable quantification of the amount and variability of evapotranspiration (ET) on the Tibetan...