{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,12,19]],"date-time":"2025-12-19T15:49:48Z","timestamp":1766159388427,"version":"build-2065373602"},"reference-count":70,"publisher":"MDPI AG","issue":"6","license":[{"start":{"date-parts":[[2024,3,15]],"date-time":"2024-03-15T00:00:00Z","timestamp":1710460800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"National Natural Science Foundation of China","award":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"],"award-info":[{"award-number":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"]}]},{"name":"Natural Science Basic Research Program of Shaanxi","award":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"],"award-info":[{"award-number":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"]}]},{"name":"Open Fund of Wuhan Gravitation and Solid Earth Tides National Observation and Research Station","award":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"],"award-info":[{"award-number":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"]}]},{"name":"Xianyang Key Research and Development Program of Chain","award":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"],"award-info":[{"award-number":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"]}]},{"name":"State Key Laboratory of Earthquake Dynamics","award":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"],"award-info":[{"award-number":["42174054","42304020","42104003","2022JZ-17","WHYWZ202202","L2023-ZDYF-SF-006","LED2022B02"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>The southeastern Tibetan Plateau (SETP), which hosts the most extensive marine glaciers on the Tibetan Plateau (TP), exhibits enhanced sensitivity to climatic fluctuations. Under global warming, persistent glacier mass depletion within the SETP poses a risk to water resource security and sustainability in adjacent nations and regions. This study deployed a high-precision ICESat-2 satellite altimetry technique to evaluate SETP glacier thickness changes from 2018 to 2022. Our results show that the average change rate in glacier thickness in the SETP is \u22120.91 \u00b1 0.18 m\/yr, and the corresponding glacier mass change is \u22127.61 \u00b1 1.52 Gt\/yr. In the SETP, the glacier mass loss obtained via ICESat-2 data is larger than the mass change in total land water storage observed by the Gravity Recovery and Climate Experiment follow-on satellite (GRACE-FO), \u22125.13 \u00b1 2.55 Gt\/yr, which underscores the changes occurring in other land water components, including snow (\u22120.44 \u00b1 0.09 Gt\/yr), lakes (\u22120.06 \u00b1 0.02 Gt\/yr), soil moisture (1.88 \u00b1 1.83 Gt\/yr), and groundwater (1.45 \u00b1 0.70 Gt\/yr), with a closure error of \u22120.35 Gt\/yr. This demonstrates that this dramatic glacier mass loss is the main reason for the decrease in total land water storage in the SETP. Generally, there are decreasing trends in solid water storage (glacier and snow) against stable or increasing trends in liquid water storage (lakes, soil moisture, and groundwater) in the SETP. This persistent decrease in solid water is linked to the enhanced melting induced by rising temperatures. Given the decreasing trend in summer precipitation, the surge in liquid water in the SETP should be principally ascribed to the increased melting of solid water.<\/jats:p>","DOI":"10.3390\/rs16061048","type":"journal-article","created":{"date-parts":[[2024,3,15]],"date-time":"2024-03-15T12:02:39Z","timestamp":1710504159000},"page":"1048","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":8,"title":["Glacier Mass Balance and Its Impact on Land Water Storage in the Southeastern Tibetan Plateau Revealed by ICESat-2 and GRACE-FO"],"prefix":"10.3390","volume":"16","author":[{"given":"Jinwei","family":"Tong","sequence":"first","affiliation":[{"name":"College of Geological Engineering and Geomatics, Chang\u2019an University, Xi\u2019an 710054, China"}]},{"given":"Zhen","family":"Shi","sequence":"additional","affiliation":[{"name":"College of Geological Engineering and Geomatics, Chang\u2019an University, Xi\u2019an 710054, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7915-0575","authenticated-orcid":false,"given":"Jiashuang","family":"Jiao","sequence":"additional","affiliation":[{"name":"Wuhan Gravitation and Solid Earth Tides National Observation and Research Station, Wuhan 430071, China"},{"name":"School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-3214-977X","authenticated-orcid":false,"given":"Bing","family":"Yang","sequence":"additional","affiliation":[{"name":"College of Geological Engineering and Geomatics, Chang\u2019an University, Xi\u2019an 710054, China"}]},{"given":"Zhen","family":"Tian","sequence":"additional","affiliation":[{"name":"College of Geological Engineering and Geomatics, Chang\u2019an University, Xi\u2019an 710054, China"}]}],"member":"1968","published-online":{"date-parts":[[2024,3,15]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"663","DOI":"10.1038\/nclimate1580","article-title":"Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings","volume":"2","author":"Yao","year":"2012","journal-title":"Nat. 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