Articles | Volume 16, issue 2
Clim. Past, 16, 555–573, 2020
Clim. Past, 16, 555–573, 2020

Research article 19 Mar 2020

Research article | 19 Mar 2020

Changes in the high-latitude Southern Hemisphere through the Eocene–Oligocene transition: a model–data comparison

Alan T. Kennedy-Asser et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (13 Jan 2020) by Yannick Donnadieu
AR by Anna Wenzel on behalf of the Authors (23 Jan 2020)  Author's response    Manuscript
ED: Publish as is (11 Feb 2020) by Yannick Donnadieu
Short summary
Global cooling and a major expansion of ice over Antarctica occurred ~ 34 million years ago at the Eocene–Oligocene transition (EOT). A large secondary proxy dataset for high-latitude Southern Hemisphere temperature before, after and across the EOT is compiled and compared to simulations from two coupled climate models. Although there are inconsistencies between the models and data, the comparison shows amongst other things that changes in the Drake Passage were unlikely the cause of the EOT.