Is a warming of the Antarctic continental shelf reversible?
IPCC-AR4 scenario forced simulations with the coupled sea ice - ice shelf - ocean models (BRIOS and FESOM) show a strong sensitivity of the southern Weddell Sea to the freshwater fluxes resulting from the atmospheric forcing and related sea ice formation. As a consequence of continues freshening dur...
| Main Authors: | , , |
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| Format: | Conference Object |
| Language: | unknown |
| Published: |
2014
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/36425/ https://hdl.handle.net/10013/epic.44259 |