Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Glacier Mass Balance Pattern and Its Variation Mechanism in the West Kunlun Mountains in Tibetan Plateau | |
Gao, Le1,2,3; Yang, Xiaofeng4; Qi, Jifeng1,2,3; Chen, Wenfeng5 | |
2022-06-01 | |
发表期刊 | REMOTE SENSING |
卷号 | 14期号:11页码:16 |
通讯作者 | Yang, Xiaofeng([email protected]) |
摘要 | Mass balance observations are beneficial for assessing climate change in different world regions. This study analyzed the glacier elevation change, ice flux divergence, and surface mass balance (SMB) in the West Kunlun Mountains (WKM) on the Tibetan Plateau using remote sensing data, including satellite altimetry, glacier surface velocity, and thickness fields. Seventeen local glaciers were examined in detail and showed varying surface elevation changes from -0.39 +/- 0.11 to 0.83 +/- 0.10 m/a. Overall, we obtained a reasonably rapid elevation trend of 0.21 +/- 0.14 m/a. By combining the ice flux divergence and surface mass balance, the overall thickness change of the WKM glacier over time is almost zero, and the WKM glacier shows a positive mass balance of 0.21 +/- 0.98 m/a. Moreover, the ice flux divergence is more significant on the ice tongue than in the flat region due to the more considerable gradient of surface velocity and thickness fields. We found that glacier heterogeneity dynamics were associated with a surging dynamic mechanism concentrated in the glacier tongue and were induced by inner terrain instabilities. The glacier surging causes a drastic drop in glacier elevation but does not cause a glacier mass gain or loss, and it has an enhanced effect on the ice flux divergence. Therefore, glacier surging is the main reason for the decline of the two glaciers monitored. In addition, the long-term meteorological data analysis found that, since 2000, the air temperature warming hiatus may have balanced the three glaciers, and significantly increasing precipitation variation may cause the glacier to thicken the most. |
关键词 | satellite altimetry glacier elevation change glacier inner terrain glacier surging ice flux divergence surface mass balance climate change |
DOI | 10.3390/rs14112634 |
收录类别 | SCI |
语种 | 英语 |
资助项目 | National Natural Science Foundation of China[42090044]; National Natural Science Foundation of China[U2006211]; Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao)[2022QNLM050301-2]; Natural Science Foundation of Shandong Province, China[ZR2021MD022]; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA19060101]; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42000000]; Major scientific and technological innovation projects in Shandong Province[2019JZZY010102]; CAS Program[Y9KY04101L] |
WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS类目 | Environmental Sciences ; Geosciences, Multidisciplinary ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS记录号 | WOS:000809005700001 |
出版者 | MDPI |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/179525 |
专题 | 海洋环流与波动重点实验室 |
通讯作者 | Yang, Xiaofeng |
作者单位 | 1.Chinese Acad Sci, CAS Key Laboratary Ocean Circulat & Waves, Inst Oceanol, 7 Nanhai Rd, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Ctr Ocean Mega Sci, 7 Nanhai Rd, Qingdao 266071, Peoples R China 3.Pilot Natl Lab Marine Sci & Technol Qingdao, 1 Wenhai Rd, Qingdao 266237, Peoples R China 4.Chinese Acad Sci, Aerosp Informat Res Inst, State Key Lab Remote Sensing Sci, Beijing 100101, Peoples R China 5.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Resource, Beijing 100101, Peoples R China |
第一作者单位 | 中国科学院海洋研究所 |
推荐引用方式 GB/T 7714 | Gao, Le,Yang, Xiaofeng,Qi, Jifeng,et al. Glacier Mass Balance Pattern and Its Variation Mechanism in the West Kunlun Mountains in Tibetan Plateau[J]. REMOTE SENSING,2022,14(11):16. |
APA | Gao, Le,Yang, Xiaofeng,Qi, Jifeng,&Chen, Wenfeng.(2022).Glacier Mass Balance Pattern and Its Variation Mechanism in the West Kunlun Mountains in Tibetan Plateau.REMOTE SENSING,14(11),16. |
MLA | Gao, Le,et al."Glacier Mass Balance Pattern and Its Variation Mechanism in the West Kunlun Mountains in Tibetan Plateau".REMOTE SENSING 14.11(2022):16. |
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文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
remotesensing-14-026(18087KB) | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 |
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