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Pathways of ocean heat towards Pine Island and Thwaites grounding lines
In the Amundsen Sea, modified Circumpolar Deep Water (mCDW) intrudes into ice shelf cavities, causing high ice shelf melting near the ice sheet grounding lines, accelerating ice flow, and controlling the pace of future Antarctic contributions to global sea level. The pathways of mCDW towards groundi...
Guardat en:
| Publicat a: | Sci Rep |
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| Autors principals: | , , , , , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2019
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6874652/ https://ncbi.nlm.nih.gov/pubmed/31757979 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-53190-6 |
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