Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-153-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-15-153-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
24 Jan 2019
Research article | Highlight paper |
| 24 Jan 2019
| 24 Jan 2019
Heinrich events show two-stage climate response in transient glacial simulations
Florian Andreas Ziemen
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Bundesstraße 53,
20146 Hamburg, Germany
Marie-Luise Kapsch
Max Planck Institute for Meteorology, Bundesstraße 53,
20146 Hamburg, Germany
Marlene Klockmann
Max Planck Institute for Meteorology, Bundesstraße 53,
20146 Hamburg, Germany
Uwe Mikolajewicz
Max Planck Institute for Meteorology, Bundesstraße 53,
20146 Hamburg, Germany
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Latest update: 18 Apr 2024
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.
Heinrich events are among the dominant modes of glacial climate variability. They are caused by...
