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Data Center","award":["2022xjkk0701"],"award-info":[{"award-number":["2022xjkk0701"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["2022xjkk0802"],"award-info":[{"award-number":["2022xjkk0802"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["42001066"],"award-info":[{"award-number":["42001066"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["42001067"],"award-info":[{"award-number":["42001067"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["SKLCS-ZZ-2022"],"award-info":[{"award-number":["SKLCS-ZZ-2022"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["20D05"],"award-info":[{"award-number":["20D05"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["Y2021110"],"award-info":[{"award-number":["Y2021110"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["2021xjkk14001"],"award-info":[{"award-number":["2021xjkk14001"]}]},{"name":"Youth Innovation Promotion Association of Chinese Academy of Sciences","award":["2022xjkk0701"],"award-info":[{"award-number":["2022xjkk0701"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["2022xjkk0802"],"award-info":[{"award-number":["2022xjkk0802"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["42001066"],"award-info":[{"award-number":["42001066"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["42001067"],"award-info":[{"award-number":["42001067"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["SKLCS-ZZ-2022"],"award-info":[{"award-number":["SKLCS-ZZ-2022"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["20D05"],"award-info":[{"award-number":["20D05"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["Y2021110"],"award-info":[{"award-number":["Y2021110"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["2021xjkk14001"],"award-info":[{"award-number":["2021xjkk14001"]}]},{"name":"Third Xinjiang Scientific Expedition (TXSE) program","award":["2022xjkk0701"],"award-info":[{"award-number":["2022xjkk0701"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>The Mt.Tomur glaciers, in the Tian Shan mountains of Western China, are usually debris-covered, and due to climate change, glacial hazards are becoming more frequent in this region. However, no changes in the long-time series of glacier surface velocities have been observed in this region. Conducting field measurements in high-altitude mountains is relatively difficult, and consequently, the dynamics and driving factors are less studied. Here, image-correlation offset tracking using Landsat images was exploited to estimate the glacier surface velocity of glaciers in the Mt.Tomur region from 2000 to 2020 and to assess glacier ice thickness. The results show that the glacier surface velocity in the Mt.Tomur region showed a significant slowdown during 2000\u20132020, from 6.71 \u00b1 0.66 m a\u22121 to 3.95 \u00b1 0.66 m a\u22121, an overall decrease of 41.13%. The maximum glacier ice thickness in the Mt.Tomur region was estimated based on the ice flow principle being 171.27 \u00b1 17.10 m, and the glacier average thickness is 50.00 \u00b1 5.0 m. Glacier thickness at first increases with increasing altitude, showing more than 100 \u00b1 10 m ice thickness between 3400 m and 4300 m, and then decreases with further increases in altitude. The reliability of the surface velocity and ice thickness obtained from remote sensing was proved using the measured surface velocity and ice thickness of Qingbingtan glacier No. 72 stall (the correlation coefficient R2 &gt; 0.85). The debris cover has an overall mitigating effect on the ablation and movement rate of Qingbingtan Glacier No. 72; however, it has an accelerating effect on the ablation and movement rate of glacier No. 74.<\/jats:p>","DOI":"10.3390\/rs15010150","type":"journal-article","created":{"date-parts":[[2022,12,28]],"date-time":"2022-12-28T05:30:27Z","timestamp":1672205427000},"page":"150","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":13,"title":["Dynamic Monitoring of Debris-Covered Glacier Surface Velocity and Ice Thickness of Mt.Tomur, Tian Shan, China"],"prefix":"10.3390","volume":"15","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-4409-3811","authenticated-orcid":false,"given":"Changbin","family":"Bai","sequence":"first","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"},{"name":"University of Chinese Academy of Sciences, Beijing 100049, China"}]},{"given":"Feiteng","family":"Wang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"},{"name":"University of Chinese Academy of Sciences, Beijing 100049, China"}]},{"given":"Lin","family":"Wang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-4803-1995","authenticated-orcid":false,"given":"Chunhai","family":"Xu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4672-8059","authenticated-orcid":false,"given":"Xiaoying","family":"Yue","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]},{"given":"Shujing","family":"Yang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]},{"given":"Puyu","family":"Wang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"},{"name":"University of Chinese Academy of Sciences, Beijing 100049, China"}]},{"given":"Yanqun","family":"Bi","sequence":"additional","affiliation":[{"name":"Guangxi Water & Power Design Institute Co., Ltd., Nanning 530000, China"}]},{"given":"Haining","family":"Wei","sequence":"additional","affiliation":[{"name":"Guangxi Water & Power Design Institute Co., Ltd., Nanning 530000, China"}]}],"member":"1968","published-online":{"date-parts":[[2022,12,27]]},"reference":[{"key":"ref_1","first-page":"581","article-title":"Relationship between the glacier and climate change in the Altun Mountain in recent four decades","volume":"40","author":"Fansheng","year":"2017","journal-title":"Arid Land Geogr."},{"key":"ref_2","first-page":"1402","article-title":"Glacier changes in the Qinlian Mountains in the past half century: Based on the revised First and Second Chinese Glacier Inventory","volume":"70","author":"Sun","year":"2015","journal-title":"Acta Geogr. 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