Response of soil hydrothermal processes within the active layer to variable alpine vegetation conditions on the Qinghai‒Tibet Plateau-Reference-Cited by-同舟云学术

Response of soil hydrothermal processes within the active layer to variable alpine vegetation conditions on the Qinghai‒Tibet Plateau

Published:2023-04 Issue:2 Volume:14 Page:200-212
ISSN:1674-9278
Container-title:Advances in Climate Change Research
language:en
Short-container-title:Advances in Climate Change Research

Author:

Fu Zi-Teng,Wu Qing-Bai,Wang Lu-Yang^ORCID,Liu Ya-Li

Publisher

Elsevier BV

Subject

Management, Monitoring, Policy and Law,Atmospheric Science,Global and Planetary Change

Reference82 articles.

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1. Summer heat wave in 2022 led to rapid warming of permafrost in the central Qinghai-Tibet Plateau;npj Climate and Atmospheric Science;2024-09-13

2. Response of soil hydrothermal processes within the active layer to variable alpine vegetation in the Yangtze River Source Area, Qinghai-Tibet plateau;Journal of Hydrology: Regional Studies;2024-08

3. Effects of vegetation extreme degradation on soil hydrothermal processes in alpine wet meadow on the central Qinghai–Tibet Plateau;Cold Regions Science and Technology;2024-08

4. Thermal and hydrological processes in permafrost slope wetlands affect thermosyphon embankment stability;Advances in Climate Change Research;2024-08

5. Permafrost temperature dynamics and its climate relations in various Tibetan alpine grasslands;CATENA;2024-06