North Atlantic ocean circulation and abrupt climate change during the last glaciation.
The most recent ice age was characterized by rapid and hemispherically asynchronous climate oscillations, whose origin remains unresolved. Variations in oceanic meridional heat transport may contribute to these repeated climate changes, which were most pronounced during marine isotope stage 3, the g...
Main Authors: | , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
2016
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Subjects: | |
Online Access: | https://www.repository.cam.ac.uk/handle/1810/296364 https://doi.org/10.17863/CAM.43413 |