Kinematic response of ice-rise divides to changes in ocean and atmosphere forcing
<p>The majority of Antarctic ice shelves are bounded by grounded ice rises. These ice rises exhibit local flow fields that partially oppose the flow of the surrounding ice shelves. Formation of ice rises is accompanied by a characteristic upward-arching internal stratigraphy (“Raymond arches”)...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-10-01
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| Series: | The Cryosphere |
| Online Access: | https://www.the-cryosphere.net/13/2673/2019/tc-13-2673-2019.pdf |