Articles | Volume 13, issue 1
https://doi.org/10.5194/tc-13-219-2019
© Author(s) 2019. 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-13-219-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
24 Jan 2019
Research article |
| 24 Jan 2019
| 24 Jan 2019
Characterizing the behaviour of surge- and non-surge-type glaciers in the Kingata Mountains, eastern Pamir, from 1999 to 2016
Mingyang Lv
School of Earth Sciences and Engineering, Nanjing University,
Nanjing, 210023, China
Key Laboratory of Digital Earth Science,
Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences,
Beijing, 100094, China
School of Geography, University of Leeds, Leeds, LS2 9JT,
UK
Huadong Guo
School of Earth Sciences and Engineering, Nanjing University,
Nanjing, 210023, China
Key Laboratory of Digital Earth Science,
Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences,
Beijing, 100094, China
Xiancai Lu
School of Earth Sciences and Engineering, Nanjing University,
Nanjing, 210023, China
Guang Liu
CORRESPONDING AUTHOR
Key Laboratory of Digital Earth Science,
Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences,
Beijing, 100094, China
Shiyong Yan
Jiangsu Key Laboratory of Resources and
Environmental Engineering, School of Environment Science and Spatial
Informatics, China University of Mining and Technology, Xuzhou, 221116,
China
Zhixing Ruan
Key Laboratory of Digital Earth Science,
Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences,
Beijing, 100094, China
Yixing Ding
Key Laboratory of Digital Earth Science,
Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences,
Beijing, 100094, China
Duncan J. Quincey
School of Geography, University of Leeds, Leeds, LS2 9JT,
UK
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Short summary
We highlight 28 glaciers in the Kingata Mountains, among which 17 have changed markedly over the last decade. We identify four advancing and 13 surge-type glaciers. The dynamic evolution of the surges is similar to that of Karakoram, suggesting that both hydrological and thermal controls are important for surge initiation and recession. Topography seems to be a dominant control on non-surge glacier behaviour. Most glaciers experienced a significant and diverse change in their motion patterns.
We highlight 28 glaciers in the Kingata Mountains, among which 17 have changed markedly over the...
