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Rapid Red Sea Deep Water renewals caused by volcanic eruptions and the North Atlantic Oscillation
The Red Sea hosts a deep marine environment unique among the world’s oceans. It is occupied, almost homogeneously from the subsurface (~137 to 300 m) to depths over 2000 m, by a warm (~21.5°C) and highly saline (~40.5) water mass, referred to as the Red Sea Deep Water (RSDW). Previous studies sugges...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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American Association for the Advancement of Science
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6021143/ https://www.ncbi.nlm.nih.gov/pubmed/29963625 http://dx.doi.org/10.1126/sciadv.aar5637 |