Arctic Ocean sea ice response to Northern Annular Mode-like wind forcing

The response of the Arctic Ocean sea ice system to Northern Annular Mode-like wind forcing has been investigated using an ocean/sea ice general circulation model coupled to an atmospheric boundary layer model. A series of idealized experiments was performed to investigate the Arctic Ocean's res...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Krahmann, Gerd, Visbeck, Martin
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2003
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/489/
https://oceanrep.geomar.de/id/eprint/489/1/2003GL017354.pdf
https://doi.org/10.1029/2003GL017354
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Summary:The response of the Arctic Ocean sea ice system to Northern Annular Mode-like wind forcing has been investigated using an ocean/sea ice general circulation model coupled to an atmospheric boundary layer model. A series of idealized experiments was performed to investigate the Arctic Ocean's response to idealized winter wind anomalies on interannual to multi-decadal time scales. The sea ice response of the model consists of a rapid change of ice movements leading to widespread variation in sea ice thickness and concentration. In most areas the response is largely independent of the forcing frequency with only a slight increase towards longer periods. Only the Greenland Sea exhibited a change in sign of sea ice concentration anomalies at about 20 years period which appears to be caused by slow adjustment of the oceanic circulation.