Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021
Glacier mass balance is one of the most direct indicators reflecting corresponding climate change. In the context of global warming, most glaciers are melting and receding, which can have significant impacts on ecology, climate, and water resources. Thus, it is important to study glacier mass change...
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MDPI AG
2022-12-01
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Online Access: | https://www.mdpi.com/2072-4292/14/24/6281 |
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author | Drolma Lhakpa Yubin Fan Yu Cai |
author_facet | Drolma Lhakpa Yubin Fan Yu Cai |
author_sort | Drolma Lhakpa |
collection | DOAJ |
description | Glacier mass balance is one of the most direct indicators reflecting corresponding climate change. In the context of global warming, most glaciers are melting and receding, which can have significant impacts on ecology, climate, and water resources. Thus, it is important to study glacier mass change, in order to assess and project its variations from past to future. Here, the Karakoram, one of the most concentrated glacierized areas in High-Mountain Asia (HMA), was selected as the study area. This study utilized SRTM<sub>-C</sub> DEM and ICESat-2 to investigate glacier mass change in the Karakoram, and its response to climatic and topographical factors during 2000–2021. The results of the data investigation showed that, overall, the “Karakoram Anomaly” still exists, with an annual averaged mass change rate of 0.02 ± 0.09 m w.e.yr<sup>-1</sup>. In different sub-regions, it was found that the western and central Karakoram glaciers gained ice mass, while the eastern Karakoram glaciers lost ice mass in the past two decades. In addition, it was discovered that the increasing precipitation trend is leading to mass gains in the western and central Karakoram glaciers, whereas increasing temperature is causing ice mass loss in the eastern Karakoram glacier. Generally, decreasing net shortwave radiation and increasing cloud cover in the Karakoram restricts ice mass loss, while topographical shading and debris cover also have dominant impacts on glacier mass change. |
first_indexed | 2024-03-09T15:54:36Z |
format | Article |
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issn | 2072-4292 |
language | English |
last_indexed | 2024-03-09T15:54:36Z |
publishDate | 2022-12-01 |
publisher | MDPI AG |
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series | Remote Sensing |
spelling | doaj.art-89ae24029f15473085c9ed53657be17a2023-11-24T17:47:07ZengMDPI AGRemote Sensing2072-42922022-12-011424628110.3390/rs14246281Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021Drolma Lhakpa0Yubin Fan1Yu Cai2Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing 210023, ChinaJiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing 210023, ChinaJiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing 210023, ChinaGlacier mass balance is one of the most direct indicators reflecting corresponding climate change. In the context of global warming, most glaciers are melting and receding, which can have significant impacts on ecology, climate, and water resources. Thus, it is important to study glacier mass change, in order to assess and project its variations from past to future. Here, the Karakoram, one of the most concentrated glacierized areas in High-Mountain Asia (HMA), was selected as the study area. This study utilized SRTM<sub>-C</sub> DEM and ICESat-2 to investigate glacier mass change in the Karakoram, and its response to climatic and topographical factors during 2000–2021. The results of the data investigation showed that, overall, the “Karakoram Anomaly” still exists, with an annual averaged mass change rate of 0.02 ± 0.09 m w.e.yr<sup>-1</sup>. In different sub-regions, it was found that the western and central Karakoram glaciers gained ice mass, while the eastern Karakoram glaciers lost ice mass in the past two decades. In addition, it was discovered that the increasing precipitation trend is leading to mass gains in the western and central Karakoram glaciers, whereas increasing temperature is causing ice mass loss in the eastern Karakoram glacier. Generally, decreasing net shortwave radiation and increasing cloud cover in the Karakoram restricts ice mass loss, while topographical shading and debris cover also have dominant impacts on glacier mass change.https://www.mdpi.com/2072-4292/14/24/6281glacier mass balanceICESat-2SRTMdriving factorsKarakoram Mountains |
spellingShingle | Drolma Lhakpa Yubin Fan Yu Cai Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021 Remote Sensing glacier mass balance ICESat-2 SRTM driving factors Karakoram Mountains |
title | Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021 |
title_full | Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021 |
title_fullStr | Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021 |
title_full_unstemmed | Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021 |
title_short | Continuous Karakoram Glacier Anomaly and Its Response to Climate Change during 2000–2021 |
title_sort | continuous karakoram glacier anomaly and its response to climate change during 2000 2021 |
topic | glacier mass balance ICESat-2 SRTM driving factors Karakoram Mountains |
url | https://www.mdpi.com/2072-4292/14/24/6281 |
work_keys_str_mv | AT drolmalhakpa continuouskarakoramglacieranomalyanditsresponsetoclimatechangeduring20002021 AT yubinfan continuouskarakoramglacieranomalyanditsresponsetoclimatechangeduring20002021 AT yucai continuouskarakoramglacieranomalyanditsresponsetoclimatechangeduring20002021 |