Differential response to rainfall of soil moisture infiltration in permafrost and seasonally frozen ground in Kangqiong small basin on the Qinghai-Tibet Plateau
Author:
Affiliation:
1. State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China
Funder
National Natural Science Foundation of China
Publisher
Informa UK Limited
Subject
Water Science and Technology
Link
https://www.tandfonline.com/doi/pdf/10.1080/02626667.2021.1883619
Reference38 articles.
1. Climatic and associated cryospheric, biospheric, and hydrological changes on the Tibetan Plateau: a review
2. Spatial variability and its main controlling factors of the permafrost soil-moisture on the northern-slope of Bayan Har Mountains in Qinghai-Tibet Plateau
3. Seasonal dynamics of suprapermafrost groundwater and its response to the freeing-thawing processes of soil in the permafrost region of Qinghai-Tibet Plateau
4. Review: Progress in permafrost hydrogeology in China
5. Permafrost and groundwater on the Qinghai-Tibet Plateau and in northeast China
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