Evolution of Ocean circulation in the North Atlantic Ocean during the Miocene: impact of the Greenland ice sheet and the Eastern Tethys Seaway
International audience The Atlantic Meridional Overturning Circulation (AMOC) is today the central feature of the Global ocean circulation (Talley, 2013). It is dominated by two overturning cells usually referred to as the Antarctic Bottom Water (AABW) and the North Atlantic Deep Water (NADW). The N...
Published in: | Paleoceanography and Paleoclimatology |
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Main Authors: | , , , , |
Other Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2022
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Subjects: | |
Online Access: | https://hal.science/hal-03763405 https://hal.science/hal-03763405/document https://hal.science/hal-03763405/file/Paleoceanog%20and%20Paleoclimatol%20-%202022%20-%20Pillot%20-%20Evolution%20of%20Ocean%20Circulation%20in%20the%20North%20Atlantic%20Ocean%20During%20the.pdf https://doi.org/10.1029/2022pa004415 |