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Bulletin of Chinese Academy of Sciences (Chinese Version)

Authors

ZHAO Lin, School of Geographical Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China
HU Guojie, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
ZOU Defu, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
WU Xiaodong, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
MA Lu, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; University of Chinese Academy of Sciences, Beijing 100049, China
SUN Zhe, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; University of Chinese Academy of Sciences, Beijing 100049, China
YUAN Liming, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; University of Chinese Academy of Sciences, Beijing 100049, China
ZHOU Huayun, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; University of Chinese Academy of Sciences, Beijing 100049, China
LIU Shibo, Cryosphere Research Station on Qinghai-Xizang Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; University of Chinese Academy of Sciences, Beijing 100049, China

Keywords

permafrost; active layer; temperature; soil moisture content; precipitation

Document Type

Article

Abstract

Under the background of global warming, permafrost on the Qinghai-Tibet Plateau has been experienced a significant degradation, which may have effects on regional climate, hydrological and ecological processes. Based on long-term observation data in permafrost region of Qinghai-Tibet Plateau and reanalysis data, the variation characteristics of temperature and precipitation in permafrost region in recent ten years were analyzed, and the variation trends of active layer thickness, ground temperature and soil water content were examined in this study. The spatial and temporal distribution of precipitation and soil water content in permafrost region from 1980 to 2018 were presented. The results showed that the permafrost in different regions on the Qinghai-Tibet Plateau has changed significantly in the past ten years. The thickness of the active layer and the ground temperature has increased, and the soil water content at the bottom of the active layer has increased. At the regional scale, the precipitation and soil water content in permafrost region increased significantly from 1980 to 2018. The possible impacts of permafrost degradation on hydrological processes, lake area changes and surface deformation were discussed. The results are helpful to understand the impact of permafrost changes on regional environment, deepen our understanding of the mechanisms of the interaction between permafrost and water cycle, and provide a scientific basis for environmental protection, engineering design and construction in cold regions.

First page

1233

Last Page

1246

Language

Chinese

Publisher

Bulletin of Chinese Academy of Sciences

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