Articles | Volume 30, issue 19
https://doi.org/10.5194/hess-30-6249-2026
https://doi.org/10.5194/hess-30-6249-2026
Research article
 | 
09 Oct 2026
Research article |  | 09 Oct 2026

The influence of vapor pressure deficit changes on global terrestrial evapotranspiration

Yuxin Miao, Guofeng Zhu, Yuhao Wang, Enwei Huang, Qingyang Wang, Yani Gun, Zhijie Zheng, Jiangwei Yang, Wenmin Li, and Ziwen Liu

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Cited articles

Bai, H., Zhong, Y., Ma, N., Kong, D., Mao, Y., Feng, W., Wu, Y., and Zhong, M.: Changes and drivers of long-term land evapotranspiration in the Yangtze River Basin: A water balance perspective, J. Hydrol., 653, 132763, https://doi.org/10.1016/j.jhydrol.2025.132763, 2025. 
Brunner, M. I. and Naveau, P.: Spatial variability in Alpine reservoir regulation: deriving reservoir operations from streamflow using generalized additive models, Hydrol. Earth Syst. Sci., 27, 673–687, https://doi.org/10.5194/hess-27-673-2023, 2023. 
Cao, S., Li, M., Zhu, Z., Wang, Z., Zha, J., Zhao, W., Duanmu, Z., Chen, J., Zheng, Y., Chen, Y., Myneni, R. B., and Piao, S.: Spatiotemporally consistent global dataset of the GIMMS leaf area index (GIMMS LAI4g) from 1982 to 2020, Earth Syst. Sci. Data, 15, 4877–4899, https://doi.org/10.5194/essd-15-4877-2023, 2023a. 
Cao, S., Li, M., Zhu, Z., Wang, Z., Zha, J., Zhao, W., Duanmu, Z., Chen, J., Zheng, Y., Chen, Y., Myneni, R. B., and Piao, S.: Spatiotemporally consistent global dataset of the GIMMS Leaf Area Index (GIMMS LAI4g) from 1982 to 2020 (V1.2) (Version V1.2), Zenodo [data set], https://doi.org/10.5281/zenodo.8281930, 2023b. 
Chai, Y., Yue, Y., Slater, L., and Miao, C.: Emergent constraints indicate slower increases in future global evapotranspiration, npj Clim. Atmos. Sci., 8, 46, https://doi.org/10.1038/s41612-025-00932-1, 2025. 
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As the climate warms, drier air can change how water moves from land to the atmosphere. We used global satellite and climate data from 1981 to 2020 to study this change. We found that drier air was linked to greater water loss over about 61% of land, especially in warm and humid regions. Plant water loss was more strongly linked to air dryness than water loss from bare soil, while dry regions showed limits or declines. These results can improve forecasts of future water-cycle change.
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