Articles | Volume 12, issue 1
https://doi.org/10.5194/tc-12-103-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-12-103-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
12 Jan 2018
Research article |
| 12 Jan 2018
| 12 Jan 2018
Recent glacier mass balance and area changes in the Kangri Karpo Mountains from DEMs and glacier inventories
School of Resources and Environment, Anqing Normal University, Anqing, 246133, China
Institute of International Rivers and Eco-Security, Yunnan University, Kunming, 650091, China
Institute of International Rivers and Eco-Security, Yunnan University, Kunming, 650091, China
State key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China
Zongli Jiang
Department of Geography, Hunan University of Science and Technology, Xiangtan, 411201, China
Junli Xu
Department of Surveying and Mapping, Yancheng Teachers University, Yancheng, 224007 China
Junfeng Wei
Department of Geography, Hunan University of Science and Technology, Xiangtan, 411201, China
Wanqin Guo
State key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China
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Latest update: 01 Nov 2024
Short summary
This study presents diminishing ice cover in the Kangri Karpo Mountains by 24.9 % ± 2.2 % or 0.71 % ± 0.06 % a−1 from 1980 to 2015 but with nine glaciers advancing. By utilizing geodetic methods, glaciers have experienced a mean mass deficit of 0.46 ± 0.08 m w.e. a−1 from 1980 to 2014. These glaciers showed slight accelerated shrinkage and significant accelerated mass loss during 2000–2015 compared to that during 1980–2000, which is consistent with the tendency of climate warming.
This study presents diminishing ice cover in the Kangri Karpo Mountains by 24.9 % ± 2.2 % or...
