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DOI | 10.5194/tc-13-2733-2019 |
Contrasting thinning patterns between lake- And land-terminating glaciers in the Bhutanese Himalaya | |
Tsutaki S.; Fujita K.; Nuimura T.; Sakai A.; Sugiyama S.; Komori J.; Tshering P. | |
发表日期 | 2019 |
ISSN | 19940416 |
EISSN | 13 |
起始页码 | 2733 |
结束页码 | 2750 |
卷号 | 13期号:10 |
英文摘要 | Despite the importance of glacial lake development in ice dynamics and glacier thinning, in situ and satellite-based measurements from lake-terminating glaciers are sparse in the Bhutanese Himalaya, where a number of proglacial lakes exist. We acquired in situ and satellite-based observations across lake- and land-terminating debris-covered glaciers in the Lunana region, Bhutanese Himalaya. A repeated differential global positioning system survey reveals that thickness change of the debris-covered ablation area of the lake-terminating Lugge Glacier (-4.67 ± 0.07ma-1) is more than 3 times more negative than that of the land-terminating Thorthormi Glacier (-1.40 ± 0.07ma-1) for the 2004-2011 period. The surface flow velocities decrease down-glacier along Thorthormi Glacier, whereas they increase from the upper part of the ablation area to the terminus of Lugge Glacier. Numerical experiments using a two-dimensional ice flow model demonstrate that the rapid thinning of Lugge Glacier is driven by both a negative surface mass balance and dynamically induced ice thinning. However, the thinning of Thorthormi Glacier is minimized by a longitudinally compressive flow regime. Multiple supraglacial ponds on Thorthormi Glacier have been expanding since 2000 and have merged into a single proglacial lake, with the glacier terminus detaching from its terminal moraine in 2011. Numerical experiments suggest that the thinning of Thorthormi Glacier will accelerate with continued proglacial lake development. © 2019 BMJ Publishing Group. All rights reserved. |
学科领域 | flow pattern; flow velocity; glacial lake; glacier dynamics; hydrological regime; ice flow; numerical model; satellite altimetry; thinning; Bhutan; Himalayas |
语种 | 英语 |
scopus关键词 | flow pattern; flow velocity; glacial lake; glacier dynamics; hydrological regime; ice flow; numerical model; satellite altimetry; thinning; Bhutan; Himalayas |
来源期刊 | The Cryosphere
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/118822 |
作者单位 | Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan; Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan; Department of Geology and Mines, Ministry of Economic Affairs, Thimphu, Bhutan; National Institute of Polar Research, Tachikawa, Japan; Tokyo Denki University, Hatoyama, Japan; Department of Modern Life, Teikyo Heisei University, Tokyo, Japan; Cryosphere Services Division, National Center for Hydrology and Meteorology, Thimphu, Bhutan |
推荐引用方式 GB/T 7714 | Tsutaki S.,Fujita K.,Nuimura T.,et al. Contrasting thinning patterns between lake- And land-terminating glaciers in the Bhutanese Himalaya[J],2019,13(10). |
APA | Tsutaki S..,Fujita K..,Nuimura T..,Sakai A..,Sugiyama S..,...&Tshering P..(2019).Contrasting thinning patterns between lake- And land-terminating glaciers in the Bhutanese Himalaya.The Cryosphere,13(10). |
MLA | Tsutaki S.,et al."Contrasting thinning patterns between lake- And land-terminating glaciers in the Bhutanese Himalaya".The Cryosphere 13.10(2019). |
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