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...

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Bibliographic Details
Main Authors: Henry, LG, McManus, JF, Curry, WB, Roberts, NL, Piotrowski, AM, Keigwin, LD
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2016
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/296364
https://doi.org/10.17863/CAM.43413