Surging Glaciers in High Mountain Asia between 1986 and 2021
High Mountain Asia (HMA) is one of the concentrated areas of surging glaciers in the world. The dynamic movement of surging glaciers not only reshapes the periglacial landscape but also has the potential to directly or indirectly trigger catastrophic events. Therefore, it is crucial to understand th...
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| Format: | Article |
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MDPI AG
2023-09-01
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| Series: | Remote Sensing |
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| Online Access: | https://www.mdpi.com/2072-4292/15/18/4595 |
| _version_ | 1797577182392877056 |
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| author | Xiaojun Yao Sugang Zhou Meiping Sun Hongyu Duan Yuan Zhang |
| author_facet | Xiaojun Yao Sugang Zhou Meiping Sun Hongyu Duan Yuan Zhang |
| author_sort | Xiaojun Yao |
| collection | DOAJ |
| description | High Mountain Asia (HMA) is one of the concentrated areas of surging glaciers in the world. The dynamic movement of surging glaciers not only reshapes the periglacial landscape but also has the potential to directly or indirectly trigger catastrophic events. Therefore, it is crucial to understand the distribution patterns, periodicities, and occurrence mechanisms of surging glaciers. Based on Landsat TM/ETM+/OLI remote sensing images from 1986 to 2021, a total of 244 surging glaciers were identified in HMA in this study, covering an area of 11,724 km<sup>2</sup> and accounting for 12.01% of the total area of glaciers in this region. There are 185 surging glaciers identified within the Karakoram Range and Pamirs, which constitute the primary mountainous regions in HMA. From 1986 to 2021, these surging glaciers advanced at least 2802 times and exhibited different temporal and spatial patterns. A total of 36 glaciers in HMA experienced 2 or more surges during this period, with the highest number observed in the Pamirs (19), followed by the Karakorum (13), with the other regions having fewer occurrences. Obvious differences exist in the surge phase and the quiescent phase of glaciers in different regions of HMA. The surge phase of surging glaciers in the Karakoram Range and Pamirs is generally short, mostly in the range of 2~6 years. The quiescent phase lasts for 5~19 years and the overall surge cycle ranges from 9 to 24 years. The complex nature of glacier surges in HMA suggests that multiple mechanisms may be at play, necessitating further research. |
| first_indexed | 2024-03-10T22:05:30Z |
| format | Article |
| id | doaj.art-7ef0d1b8fb7b4424a19e2bd6d7d9ec20 |
| institution | Directory Open Access Journal |
| issn | 2072-4292 |
| language | English |
| last_indexed | 2024-03-10T22:05:30Z |
| publishDate | 2023-09-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Remote Sensing |
| spelling | doaj.art-7ef0d1b8fb7b4424a19e2bd6d7d9ec202023-11-19T12:49:55ZengMDPI AGRemote Sensing2072-42922023-09-011518459510.3390/rs15184595Surging Glaciers in High Mountain Asia between 1986 and 2021Xiaojun Yao0Sugang Zhou1Meiping Sun2Hongyu Duan3Yuan Zhang4College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, ChinaCollege of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, ChinaCollege of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, ChinaCollege of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, ChinaCollege of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, ChinaHigh Mountain Asia (HMA) is one of the concentrated areas of surging glaciers in the world. The dynamic movement of surging glaciers not only reshapes the periglacial landscape but also has the potential to directly or indirectly trigger catastrophic events. Therefore, it is crucial to understand the distribution patterns, periodicities, and occurrence mechanisms of surging glaciers. Based on Landsat TM/ETM+/OLI remote sensing images from 1986 to 2021, a total of 244 surging glaciers were identified in HMA in this study, covering an area of 11,724 km<sup>2</sup> and accounting for 12.01% of the total area of glaciers in this region. There are 185 surging glaciers identified within the Karakoram Range and Pamirs, which constitute the primary mountainous regions in HMA. From 1986 to 2021, these surging glaciers advanced at least 2802 times and exhibited different temporal and spatial patterns. A total of 36 glaciers in HMA experienced 2 or more surges during this period, with the highest number observed in the Pamirs (19), followed by the Karakorum (13), with the other regions having fewer occurrences. Obvious differences exist in the surge phase and the quiescent phase of glaciers in different regions of HMA. The surge phase of surging glaciers in the Karakoram Range and Pamirs is generally short, mostly in the range of 2~6 years. The quiescent phase lasts for 5~19 years and the overall surge cycle ranges from 9 to 24 years. The complex nature of glacier surges in HMA suggests that multiple mechanisms may be at play, necessitating further research.https://www.mdpi.com/2072-4292/15/18/4595surging glaciersurge phasequiescent phaseHigh Mountain AsiaLandsat |
| spellingShingle | Xiaojun Yao Sugang Zhou Meiping Sun Hongyu Duan Yuan Zhang Surging Glaciers in High Mountain Asia between 1986 and 2021 Remote Sensing surging glacier surge phase quiescent phase High Mountain Asia Landsat |
| title | Surging Glaciers in High Mountain Asia between 1986 and 2021 |
| title_full | Surging Glaciers in High Mountain Asia between 1986 and 2021 |
| title_fullStr | Surging Glaciers in High Mountain Asia between 1986 and 2021 |
| title_full_unstemmed | Surging Glaciers in High Mountain Asia between 1986 and 2021 |
| title_short | Surging Glaciers in High Mountain Asia between 1986 and 2021 |
| title_sort | surging glaciers in high mountain asia between 1986 and 2021 |
| topic | surging glacier surge phase quiescent phase High Mountain Asia Landsat |
| url | https://www.mdpi.com/2072-4292/15/18/4595 |
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