The imbalance of the Asian water tower-Reference-Cited by-同舟云学术

The imbalance of the Asian water tower

Published:2022-06-07 Issue:10 Volume:3 Page:618-632
ISSN:2662-138X
Container-title:Nature Reviews Earth & Environment
language:en
Short-container-title:Nat Rev Earth Environ

Author:

Yao Tandong,Bolch Tobias^ORCID,Chen Deliang^ORCID,Gao Jing,Immerzeel Walter^ORCID,Piao Shilong^ORCID,Su Fengge,Thompson Lonnie,Wada Yoshihide^ORCID,Wang Lei^ORCID,Wang Tao^ORCID,Wu Guangjian,Xu Baiqing,Yang Wei,Zhang Guoqing^ORCID,Zhao Ping

Publisher

Springer Science and Business Media LLC

Subject

Nature and Landscape Conservation,Atmospheric Science,Earth-Surface Processes,Pollution

Link

https://www.nature.com/articles/s43017-022-00299-4.pdf

Reference174 articles.

1. Immerzeel, W. W. et al. Importance and vulnerability of the world’s water towers. Nature 577, 364–369 (2020).This work addresses the importance and vulnerability of the AWT compared with other global water towers.

2. Yao, T. et al. Recent Third Pole’s rapid warming accompanies cryospheric melt and water cycle intensification and interactions between monsoon and environment: multidisciplinary approach with observations, modeling, and analysis. B Am. Meteorol. Soc. 100, 423–444 (2019). This paper proposes a multidisciplinary framework from the viewpoint of Earth system science for addressing Third Pole environmental changes under the current unprecedented warming.

3. Chen, D. et al. Assessment of past, present and future environmental changes on the Tibetan Plateau. Chin. Sci. Bull. 60, 3025–3035 (2015).

4. Yang, K. et al. Recent climate changes over the Tibetan Plateau and their impacts on energy and water cycle: a review. Glob. Planet. Change 112, 79–91 (2014).

5. Yao, T. et al. Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nat. Clim. Change 2, 663–667 (2012). This report provides the first evidence of glacier changes driven by the Indian monsoon and westerlies: intensive retreat in the monsoon-dominant region, advance in the westerlies-dominant region and stable in between over the Third Pole.

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