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DOI10.5194/tc-11-133-2017
Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate
Banerjee A.
发表日期2017
ISSN19940416
卷号11期号:1
英文摘要Recent geodetic mass-balance measurements reveal similar thinning rates on glaciers with or without debris cover in the Himalaya-Karakoram region. This comes as a surprise as a thick debris cover reduces the surface melting significantly due to its insulating effects. Here we present arguments, supported by results from numerical flowline model simulations of idealised glaciers, that a competition between the changes in the surface mass-balance forcing and that of the emergence/submergence velocities can lead to similar thinning rates on these two types of glaciers. As the climate starts warming, the thinning rate on a debris-covered glacier is initially smaller than that on a similar debris-free glacier. Subsequently, the rate on the debris-covered glacier becomes comparable to and then larger than that on the debris-free one. The time evolution of glacier-averaged thinning rates after an initial warming is strongly controlled by the time variation of the corresponding emergence velocity profile. © 2017 Author(s).
学科领域climate effect; flow modeling; geodetic datum; glacial debris; glacier; glacier flow; mass balance; melting; numerical model; velocity profile; warming; Himalayas; Karakoram
语种英语
scopus关键词climate effect; flow modeling; geodetic datum; glacial debris; glacier; glacier flow; mass balance; melting; numerical model; velocity profile; warming; Himalayas; Karakoram
来源期刊Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/119461
作者单位Earth and Climate Science, Indian Institute of Science Education and Research, Pune, India
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Banerjee A.. Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate[J],2017,11(1).
APA Banerjee A..(2017).Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate.Cryosphere,11(1).
MLA Banerjee A.."Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate".Cryosphere 11.1(2017).
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