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Oceanographic dynamics and the end of the last interglacial in the subpolar North Atlantic
The last interglacial interval was terminated by the inception of a long, progressive glaciation that is attributed to astronomically influenced changes in the seasonal distribution of sunlight over the earth. However, the feedbacks, internal dynamics, and global teleconnections associated with decl...
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| Auteurs principaux: | , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
National Academy of Sciences
2014
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| Sujets: | |
| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4128163/ https://ncbi.nlm.nih.gov/pubmed/25049405 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1322103111 |
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