How does soil water content influence permafrost evolution on the Qinghai-Tibet Plateau under climate warming?

How does soil water content influence permafrost evolution on the Qinghai-Tibet Plateau under climate warming?

The active layer thickness (ALT) in permafrost regions regulates hydrological cycles, water sustainability, and ecosystem functions in the cryosphere and is extremely sensitive to climate change. Previous studies often focused on the impacts of rising temperature on the ALT, while the roles of soil...

Full description

Bibliographic Details
Main Authors: Fang Ji, Linfeng Fan, Xingxing Kuang, Xin Li, Bin Cao, Guodong Cheng, Yingying Yao, Chunmiao Zheng
Format: Article
Language:English
Published: IOP Publishing 2022-01-01
Series:Environmental Research Letters
Subjects:
permafrost
active layer thickness
soil water content
Qinghai-Tibet Plateau
climate change
Online Access:https://doi.org/10.1088/1748-9326/ac6c9a

Internet

https://doi.org/10.1088/1748-9326/ac6c9a

Similar Items