Large-scale instabilities of the Laurentide ice sheet simulated in a fully coupled climate-system model

Heinrich events, related to large-scale surges of the Laurentide ice sheet, represent one of the most dramatic types of abrupt climate change occurring during the last glacial. Here, using a coupled atmosphere-ocean-biosphere-ice sheet model, we simulate quasi-periodic large-scale surges from the La...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Calov, Reinhard, Ganopolski, Andrey, Petoukhov, Vladimir, Claussen, Martin, Greve, Ralf
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union
Subjects:
Glaciology
Climate dynamics
Paleoclimatology
Heinrich event
Surge
452
Ice Sheet
Online Access:http://hdl.handle.net/2115/34653
https://doi.org/10.1029/2002GL016078
Description
Summary:Heinrich events, related to large-scale surges of the Laurentide ice sheet, represent one of the most dramatic types of abrupt climate change occurring during the last glacial. Here, using a coupled atmosphere-ocean-biosphere-ice sheet model, we simulate quasi-periodic large-scale surges from the Laurentide ice sheet. The average time between simulated events is about 7,000 yrs, while the surging phase of each event lasts only several hundred years, with a total ice volume discharge corresponding to 5-10 m of sea level rise. In our model the simulated ice surges represent internal oscillations of the ice sheet. At the same time, our results suggest the possibility of a synchronization between instabilities of different ice sheets, as indicated in paleoclimate records.

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