Increasing atmospheric evaporative demand across the Tibetan plateau and implications for surface water resources

The Tibetan Plateau, known as the "Asian water tower," is a hotspot for complex hydroclimatic changes. We reveal that the previously decreasing atmospheric evaporative demand (<i>E<sub>o</sub></i> ) trend at the end of the 20<sup>th</sup> century has reversed over the last two decades. Although both wind stilling and solar dimming have persisted, their effects on <i>E</i> <sub><i>o</i></sub> rates have been overshadowed by increasing air temperatures and decreasing relative humidity, leading to a net rise in <i>E</i> <sub><i>o</i></sub> for 1980-2015. Using the empirical "top-down" Budyko approach, we estimate that across seven sub-catchments draining the Tibetan Plateau, a 10% increase in annual-averaged precipitation, assuming all other factors remain constant, would lead to a 15%-19% increase in streamflow. Conversely, a 10% increase in annual-averaged <i>E</i> <sub><i>o</i></sub> would decrease streamflow by 5%-9%. Our findings provide a deeper understanding of the accelerating hydroclimatic changes and their impact on surface water resources in the Tibetan Plateau.

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Publication Details

Journal
iScience
Published
2024-12-18
DOI
https://doi.org/10.1016/j.isci.2024.111623
Citations
5
Primary Topic
Hydrology and Watershed Management Studies
Type
article
Field-Weighted Citation Impact
1.01

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article

Increasing atmospheric evaporative demand across the Tibetan plateau and implications for surface water resources

Tim R. McVicar, Ningpeng Dong, Shiqin Xu, Dennis P. Lettenmaier et al.
5 citations
iScience
Hydrology and Watershed Management Studies
1.01
article

Increasing atmospheric evaporative demand across the Tibetan plateau and implications for surface water resources

Tim R. McVicar, Ningpeng Dong, Shiqin Xu, Dennis P. Lettenmaier, Hylke E. Beck, Akash Koppa, Pierre Gentine, Joshua B. Fisher, Matthew F. McCabe, Zhongbo Yu
article en
5 citations

Abstract

The Tibetan Plateau, known as the "Asian water tower," is a hotspot for complex hydroclimatic changes. We reveal that the previously decreasing atmospheric evaporative demand (<i>E<sub>o</sub></i> ) trend at the end of the 20<sup>th</sup> century has reversed over the last two decades. Although both wind stilling and solar dimming have persisted, their effects on <i>E</i> <sub><i>o</i></sub> rates have been overshadowed by increasing air temperatures and decreasing relative humidity, leading to a net rise in <i>E</i> <sub><i>o</i></sub> for 1980-2015. Using the empirical "top-down" Budyko approach, we estimate that across seven sub-catchments draining the Tibetan Plateau, a 10% increase in annual-averaged precipitation, assuming all other factors remain constant, would lead to a 15%-19% increase in streamflow. Conversely, a 10% increase in annual-averaged <i>E</i> <sub><i>o</i></sub> would decrease streamflow by 5%-9%. Our findings provide a deeper understanding of the accelerating hydroclimatic changes and their impact on surface water resources in the Tibetan Plateau.

iScienceVol. 28(2)
Commonwealth Scientific and Industrial Research Organisation (AU), Australian Research Council (AU), University of California, Los Angeles (US), Hohai University (CN), Chapman University (US), China Institute of Water Resources and Hydropower Research (CN), HES-SO Valais-Wallis (CH), École Polytechnique Fédérale de Lausanne (CH), King Abdullah University of Science and Technology (SA), Columbia University (US)
National Natural Science Foundation of China, King Abdullah University of Science and Technology
Clean water and sanitation
Openalex Percentile: Top 25%
Hydrology and Watershed Management Studies
1.01
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