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Mechanisms driving variability in the ocean forcing of Pine Island Glacier
Pine Island Glacier (PIG) terminates in a rapidly melting ice shelf, and ocean circulation and temperature are implicated in the retreat and growing contribution to sea level rise of PIG and nearby glaciers. However, the variability of the ocean forcing of PIG has been poorly constrained due to a la...
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| Foilsithe in: | Nat Commun |
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| Main Authors: | , , , , , , , , , |
| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe: |
Nature Publishing Group
2017
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| Ábhair: | |
| Rochtain Ar Líne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5321733/ https://ncbi.nlm.nih.gov/pubmed/28211473 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms14507 |
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