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Ocean convection linked to the recent ice edge retreat along east Greenland
Warm subtropical-origin Atlantic water flows northward across the Greenland-Scotland Ridge into the Nordic Seas, where it relinquishes heat to the atmosphere and gradually transforms into dense Atlantic-origin water. Returning southward along east Greenland, this water mass is situated beneath a lay...
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| Publicado no: | Nat Commun |
|---|---|
| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5876363/ https://ncbi.nlm.nih.gov/pubmed/29599505 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-03468-6 |
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