Articles | Volume 15, issue 1
Clim. Past, 15, 153–168, 2019
https://doi.org/10.5194/cp-15-153-2019
Clim. Past, 15, 153–168, 2019
https://doi.org/10.5194/cp-15-153-2019
Research article
 | Highlight paper
24 Jan 2019
Research article  | Highlight paper | 24 Jan 2019

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

Florian Andreas Ziemen et al.

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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.