Mechanisms driving variability in the ocean forcing of Pine Island Glacier
Pine Island Glacier terminates in a rapidly melting ice shelf and ocean conditions are believed to influence its contribution to sea level rise. Here, the authors show that variability in these ocean conditions is driven by a combination of changes in ocean circulation and local surface heat fluxes.
| Main Authors: | , , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2017-02-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms14507 |