Southern Ocean warming: Increase in basal melting and grounded ice loss
We apply a global finite element sea ice/ice shelf/ocean model (FESOM) to the Antarctic marginal seas to analyze projections of ice shelf basal melting in a warmer climate. The model is forced with the atmospheric output from two climate models: (1) the Hadley Centre Climate Model (HadCM3) and (2) M...
Main Authors: | , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2013
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/33243/ https://epic.awi.de/id/eprint/33243/1/ProgrammeandAbstracts.pdf https://hdl.handle.net/10013/epic.41732 https://hdl.handle.net/10013/epic.41732.d001 |