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Impact of warming shelf waters on ice mélange and terminus retreat at a large SE Greenland glacier

<p>By the end of 2018 Kangerlussuaq Glacier in southeast Greenland had retreated further inland than at any time in the past 80 years and its terminus was approaching a region of retrograde bed slope from where further rapid retreat would have been inevitable. Here we show that the retreat occurred...

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Bibliografiske detaljer
Principais autores: S. L. Bevan, A. J. Luckman, D. I. Benn, T. Cowton, J. Todd
Format: Artigo
Sprog:Inglês
Udgivet: Copernicus Publications 2019-09-01
Serier:The Cryosphere
Fag:
Online adgang:https://www.the-cryosphere.net/13/2303/2019/tc-13-2303-2019.pdf
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