Articles | Volume 15, issue 1
Clim. Past, 15, 153–168, 2019
Clim. Past, 15, 153–168, 2019

Research article 24 Jan 2019

Research article | 24 Jan 2019

Heinrich events show two-stage climate response in transient glacial simulations

Florian Andreas Ziemen 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: Publish subject to minor revisions (review by editor) (05 Dec 2018) by André Paul
AR by Florian Ziemen on behalf of the Authors (14 Dec 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (22 Dec 2018) by André Paul
Short summary
Heinrich events are among the dominant modes of glacial climate variability. They are caused by massive ice discharges from the Laurentide Ice Sheet into the North Atlantic. In previous studies, the climate changes were either seen as resulting from freshwater released from the melt of the discharged icebergs or by ice sheet elevation changes. With a coupled ice sheet–climate model, we show that both effects are relevant with the freshwater effects preceding the ice sheet elevation effects.