Ice–ocean interaction and calving front morphology at two west Greenland tidewater outlet glaciers
Warm, subtropical-originating Atlantic water (AW) has been identified as a primary driver of mass loss across the marine sectors of the Greenland Ice Sheet (GrIS), yet the specific processes by which this water mass interacts with and erodes the calving front of tidewater glaciers is frequently mode...
Main Authors: | , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2014-08-01
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Series: | The Cryosphere |
Online Access: | http://www.the-cryosphere.net/8/1457/2014/tc-8-1457-2014.pdf |