Is the noble gas‐based rate of ocean warming during the Younger Dryas overestimated?

Noble gases in ice cores enable reconstructions of past mean ocean temperature. A recent result from the clathrate‐containing WAIS Divide Ice Core showed tight covariation between ocean and Antarctic temperatures throughout the last deglaciation, except for the Younger Dryas interval. In the beginni...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Shackleton, S., Bereiter, B., Baggenstos, D., Bauska, T.K., Brook, E.J., Marcott, S.A., Severinghaus, J.P.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2019
Subjects:
Online Access:https://doi.org/10.1029/2019GL082971