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.
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| Auteurs principaux: | , , , , , , , , , |
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| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2017
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| Sujets: | |
| Accès en ligne: | https://doaj.org/article/6c1147c0e7004bbe9d3a3a0b37695afb |
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