Articles | Volume 26, issue 20
https://doi.org/10.5194/acp-26-15179-2026
https://doi.org/10.5194/acp-26-15179-2026
Research article
 | 
29 Oct 2026
Research article |  | 29 Oct 2026

Lake-Mountain synergy in convective clouds and precipitation over the Tibetan Plateau: a large-eddy simulation study

Kai Yang, Jinghua Chen, Tianliang Zhao, Xiangde Xu, Chunsong Lu, Shizuo Fu, Yuehan Luo, Qingjian Yang, Ziqian Liu, Zhikuan Li, Lin Wu, and Yuxiang Jin

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Cited articles

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Short summary
The Tibetan Plateau has little available moisture and energy, so convection is hard to develop. Large-eddy simulations indicates the lake promotes low-level moistening and lowers the barrier to convective initiation, produces shallow clouds and week rain. Mountain alone force lifting, yet the lack of moisture limits terrain-driven precipitation. Lake-mountain coupling is key: the mountain lifts lake-supplied moisture but also block low-level moisture transport, reshaping precipitation patterns. 
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