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Thwaites Glacier thins and retreats fastest where ice-shelf channels intersect its grounding zone

<p>Antarctic ice shelves buttress the flow of the ice sheet but are vulnerable to increased basal melting from contact with a warming ocean and increased mass loss from calving due to changing flow patterns. Channels and similar features at the bases of ice shelves have been linked to enhanced basal...

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Principais autores: A. M. Chartrand, I. M. Howat, I. R. Joughin, B. E. Smith
Format: Artigo
Jezik:Inglês
Izdano: Copernicus Publications 2024-11-01
Serija:The Cryosphere
Online dostop:https://tc.copernicus.org/articles/18/4971/2024/tc-18-4971-2024.pdf
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