Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Southern Marine Science and Engineering Guangdong Laboratory
(Guangzhou), Guangzhou 511458, China
Changwei Xie
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Xiaofan Zhu
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Wu Wang
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Ren Li
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Amin Wen
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Dong Wang
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Peiqing Lou
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Chengpeng Shang
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Yune La
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Xianhua Wei
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Xin Ma
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Yongping Qiao
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Xiaodong Wu
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Qiangqiang Pang
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
Guojie Hu
Cryosphere Research Station on the Qinghai–Tibet Plateau, State Key
Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment
and Resource, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China
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We presented an 11-year time series of meteorological, active layer, and permafrost data at the Mahan Mountain relict permafrost site in northeastern Qinghai-Tibet Plateau. From 2010 to 2020, the increasing rate of active layer thickness was 1.8 cm-year and the permafrost temperature showed slight changes. The release of those data would be helpful to understand the impacts of climate change on permafrost in relict permafrost regions and to validate the permafrost models and land surface models.
We presented an 11-year time series of meteorological, active layer, and permafrost data at the...
