The ice front as a topographic barrier for ocean heat transport
Antarctic ice shelves are the link between the Southern Ocean and the Antarctic Ice Sheet. The floating ice shelves restrain the seaward flow of the grounded ice, which is balanced by iceberg calving and ocean-induced basal melting. An increase in oceanic heat flux towards the West Antarctic ice she...
Published in: | Nature |
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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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The University of Bergen
2021
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Online Access: | https://hdl.handle.net/11250/2760582 |