中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Linking ground ice and glacier melting to lake volume change in the Dogai Coring watershed on the Tibetan Plateau

文献类型:期刊论文

作者Zhang, Zhendong; Li, Xu; Zhou, Chaodong1; Zhao, Yanhui1; Zhao, Gang1; Tang, Qiuhong1,2
刊名JOURNAL OF HYDROLOGY
出版日期2024-02-01
卷号629页码:130581
关键词Ground ice melt Glacier mass loss Lake water budget SBAS-InSAR Dogai Coring Tibetan Plateau
DOI10.1016/j.jhydrol.2023.130581
产权排序2
英文摘要The Dogai Coring Lake on the Tibetan Plateau, with widespread permafrost and glaciers in the watershed, has expanded rapidly between 2014 and 2020. However, it remains unclear how much melting water from permafrost and glaciers contributes to the increase in lake volume. This study quantifies the potential amount of water released by the melt of permafrost and glaciers, and assesses the fraction of water storage gains in the lake offset by the loss from the cryosphere (i.e., ground ice and glaciers). The small baseline subset interferometric synthetic aperture radar (SBAS-InSAR) method was used to derive the spatiotemporal changes in surface deformation, which then assisted the estimation of the potential water release from ground ice melting. The glacier mass balance was estimated using a geodetic method with ASTER DEMs. Results show that 51.3 % of the region experienced subsidence with rates in the range of 5-20 mm center dot a(-1) during 2014-2020. Ground ice melting released water at a rate of 35.1 x 10(6) m(3)center dot a(-1), accounting for similar to 19.3 % of the increase in lake volume. The glacier mass loss rate was estimated to be - 0.69 +/- 0.04 m w.e. yr(-1) (113.6 +/- 7.3 x 10(6) m(3)center dot a(-1)), contributing similar to 62.5 % to the lake volume increase. Our results show that the water storage loss in the cryosphere has largely (similar to 80 %) offset the water storage gain in the lake, suggesting that cryospheric meltwater is an important factor regulating water budget change of the lake watershed.
WOS关键词PERMAFROST THAW ; MASS BALANCES ; SELIN CO ; CLIMATE ; ELEVATION ; DYNAMICS ; BASIN ; INTERFEROMETRY ; DEGRADATION ; TEMPERATURE
WOS研究方向Engineering ; Geology ; Water Resources
WOS记录号WOS:001143479200001
源URL[http://ir.igsnrr.ac.cn/handle/311030/201688]  
专题陆地水循环及地表过程院重点实验室_外文论文
作者单位1.Beijing Jiaotong Univ, Key Lab Urban Underground Engn, Minist Educ, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Zhendong,Li, Xu,Zhou, Chaodong,et al. Linking ground ice and glacier melting to lake volume change in the Dogai Coring watershed on the Tibetan Plateau[J]. JOURNAL OF HYDROLOGY,2024,629:130581.
APA Zhang, Zhendong,Li, Xu,Zhou, Chaodong,Zhao, Yanhui,Zhao, Gang,&Tang, Qiuhong.(2024).Linking ground ice and glacier melting to lake volume change in the Dogai Coring watershed on the Tibetan Plateau.JOURNAL OF HYDROLOGY,629,130581.
MLA Zhang, Zhendong,et al."Linking ground ice and glacier melting to lake volume change in the Dogai Coring watershed on the Tibetan Plateau".JOURNAL OF HYDROLOGY 629(2024):130581.

入库方式: OAI收割

来源:地理科学与资源研究所

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