Tipping of the Filchner-Ronne and other Antarctic ice shelf cavities
Tipping of an ice shelf cavity from a cold to a warm state happens when a sustained inflow of warm Circumpolar Deep Water (CDW) or a modified variant of it replaces High Salinity Shelf Water (HSSW) and Ice Shelf Water (ISW) in a cold-water cavity. HSSW and ISW with temperatures close to or even belo...
Main Authors: | , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
EGU General Assembly 2022
2022
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/57422/ https://hdl.handle.net/10013/epic.2384d657-832f-46ff-beba-cfc1ee41c94d |