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Glacial ocean circulation and stratification explained by reduced atmospheric temperature
Earth’s climate has undergone dramatic shifts between glacial and interglacial time periods, with high-latitude temperature changes on the order of 5–10 °C. These climatic shifts have been associated with major rearrangements in the deep ocean circulation and stratification, which have likely played...
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| Publicado no: | Proc Natl Acad Sci U S A |
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| Autor principal: | |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5224371/ https://ncbi.nlm.nih.gov/pubmed/27994158 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1610438113 |
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