Changes in the Red Sea overturning circulation during Marine Isotope Stage 3
<p>The oceanography of the Red Sea is controlled by the restricted exchange of water masses with the Indian Ocean and by high evaporation rates due to the arid climate of the surrounding land areas. In the northern Red Sea, the formation of oxygen-rich subsurface water ventilates the deeper parts of...
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| Auteurs principaux: | , , , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Copernicus Publications
2024-02-01
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| Collection: | Climate of the Past |
| Accès en ligne: | https://cp.copernicus.org/articles/20/267/2024/cp-20-267-2024.pdf |
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