The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains

Glacier surges (GSs) are a manifestation of glacier instability and one of the most striking phenomena in the mountain cryosphere. Here, we utilize optical images acquired between 1973 and 2021 to map changes in glacier surface velocity and morphology and characterize differences in surface elevatio...

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Published in:Remote Sensing
Main Authors: Yongpeng Gao, Shiyin Liu, Miaomiao Qi, Xiaojun Yao, Yu Zhu, Fuming Xie, Kunpeng Wu, Muhammad Saifullah
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
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Online Access:https://doi.org/10.3390/rs14040852
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spelling ftmdpi:oai:mdpi.com:/2072-4292/14/4/852/ 2023-08-20T04:06:43+02:00 The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains Yongpeng Gao Shiyin Liu Miaomiao Qi Xiaojun Yao Yu Zhu Fuming Xie Kunpeng Wu Muhammad Saifullah 2022-02-11 application/pdf https://doi.org/10.3390/rs14040852 EN eng Multidisciplinary Digital Publishing Institute Biogeosciences Remote Sensing https://dx.doi.org/10.3390/rs14040852 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 4; Pages: 852 glacier surges Qilian Mountains thickness change glacier surface velocity surge mechanisms Text 2022 ftmdpi https://doi.org/10.3390/rs14040852 2023-08-01T04:08:06Z Glacier surges (GSs) are a manifestation of glacier instability and one of the most striking phenomena in the mountain cryosphere. Here, we utilize optical images acquired between 1973 and 2021 to map changes in glacier surface velocity and morphology and characterize differences in surface elevation using multi-source DEMs in the Tuanjie Peak (TJP), located in the Qilian Mountains (QLMs). These data provide valuable insights into the recent dynamic evolution of glaciers and hint at how they might evolve in the next few years. We identified a confirmed surge-type glacier (STG), three likely STGs, and three possible STGs. Our observations show that TJP GSs are generally long-term, although they are shorter in some cases. During the active phase, all glaciers exhibit thickened reservoir areas and thinned receiving areas, or vice-versa. The ice volume transfer was between 0.11 ± 0.13 × 107 m3 to 5.71 ± 0.69 × 107 m3. Although it was impossible to obtain integrated velocity profiles throughout the glacier surge process due to the limitations of available satellite imagery, our recent observations show that winter velocities were much higher than summer velocities, suggesting an obvious correlation between surge dynamics and glacial hydrology. However, the initiation and termination phase of GSs in this region was slow, which is similar to Svalbard-type STGs. We hypothesize that both thermal and hydrological controls are crucial. Moreover, we suggest that the regional warming trend may potentially increase glacier instability and the possibility of surge occurrence in this region. Text glacier Svalbard MDPI Open Access Publishing Svalbard Remote Sensing 14 4 852
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic glacier surges
Qilian Mountains
thickness change
glacier surface velocity
surge mechanisms
spellingShingle glacier surges
Qilian Mountains
thickness change
glacier surface velocity
surge mechanisms
Yongpeng Gao
Shiyin Liu
Miaomiao Qi
Xiaojun Yao
Yu Zhu
Fuming Xie
Kunpeng Wu
Muhammad Saifullah
The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains
topic_facet glacier surges
Qilian Mountains
thickness change
glacier surface velocity
surge mechanisms
description Glacier surges (GSs) are a manifestation of glacier instability and one of the most striking phenomena in the mountain cryosphere. Here, we utilize optical images acquired between 1973 and 2021 to map changes in glacier surface velocity and morphology and characterize differences in surface elevation using multi-source DEMs in the Tuanjie Peak (TJP), located in the Qilian Mountains (QLMs). These data provide valuable insights into the recent dynamic evolution of glaciers and hint at how they might evolve in the next few years. We identified a confirmed surge-type glacier (STG), three likely STGs, and three possible STGs. Our observations show that TJP GSs are generally long-term, although they are shorter in some cases. During the active phase, all glaciers exhibit thickened reservoir areas and thinned receiving areas, or vice-versa. The ice volume transfer was between 0.11 ± 0.13 × 107 m3 to 5.71 ± 0.69 × 107 m3. Although it was impossible to obtain integrated velocity profiles throughout the glacier surge process due to the limitations of available satellite imagery, our recent observations show that winter velocities were much higher than summer velocities, suggesting an obvious correlation between surge dynamics and glacial hydrology. However, the initiation and termination phase of GSs in this region was slow, which is similar to Svalbard-type STGs. We hypothesize that both thermal and hydrological controls are crucial. Moreover, we suggest that the regional warming trend may potentially increase glacier instability and the possibility of surge occurrence in this region.
format Text
author Yongpeng Gao
Shiyin Liu
Miaomiao Qi
Xiaojun Yao
Yu Zhu
Fuming Xie
Kunpeng Wu
Muhammad Saifullah
author_facet Yongpeng Gao
Shiyin Liu
Miaomiao Qi
Xiaojun Yao
Yu Zhu
Fuming Xie
Kunpeng Wu
Muhammad Saifullah
author_sort Yongpeng Gao
title The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains
title_short The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains
title_full The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains
title_fullStr The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains
title_full_unstemmed The Evolution of the Glacier Surges in the Tuanjie Peak, the Qilian Mountains
title_sort evolution of the glacier surges in the tuanjie peak, the qilian mountains
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/rs14040852
geographic Svalbard
geographic_facet Svalbard
genre glacier
Svalbard
genre_facet glacier
Svalbard
op_source Remote Sensing; Volume 14; Issue 4; Pages: 852
op_relation Biogeosciences Remote Sensing
https://dx.doi.org/10.3390/rs14040852
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs14040852
container_title Remote Sensing
container_volume 14
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