Response of soil hydrothermal processes within the active layer to variable alpine vegetation in the Yangtze River Source Area, Qinghai-Tibet plateau-Reference-Cited by-同舟云学术

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Response of soil hydrothermal processes within the active layer to variable alpine vegetation in the Yangtze River Source Area, Qinghai-Tibet plateau

Published:2024-08 Issue: Volume:54 Page:101850
ISSN:2214-5818
Container-title:Journal of Hydrology: Regional Studies
language:en
Short-container-title:Journal of Hydrology: Regional Studies

Author:

Yang Bin,Duan Yanghai,Zhao Jingyi,Tan Changhai,Gesang Ji-mi,Chen Long,Zhao Yanggang,Zhang Xunxun

Publisher

Elsevier BV

Reference47 articles.

1. Permafrost and groundwater on the Qinghai-Tibet Plateau and in Northeast China;Cheng;Hydrogeol. J.,2013

2. Enhancing sustainability of grassland ecosystems through ecological restoration and grazing management in an era of climate change on Qinghai-Tibetan Plateau;Dong;Agric. Ecosyst. Environ.,2020

3. Evaluation of 11 soil thermal conductivity schemes for the permafrost region of the central Qinghai-Tibet Plateau;Du;Catena,2020

4. Response of soil hydrothermal processes within the active layer to variable alpine vegetation conditions on the Qinghai3Tibet Plateau;Fu;Advances in Climate Change Research,2023

5. Permafrost hydrology of the Qinghai-Tibet Plateau: a review of processes and modeling;Gao;Front. Earth Sci.,2021

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