Is the wind stress forcing essential for the meridional overturning circulation?

[ 1 ] We use a global couple d atm osphere-ocean sea-ice model of interm ediate complexity to demonstrate that wind- forcing i s a crucial element to sustain meridional overturning flow i n t he Atlantic. Neglecting wind-stress in our multi- century-lon g simulations leads to a complete shutdown of...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Timmermann, A., Goosse, Hugues
Other Authors: UCL - SST/ELI/ELIC - Earth & Climate
Format: Article in Journal/Newspaper
Language:English
Published: 2004
Subjects:
Online Access:http://hdl.handle.net/2078.1/129619
https://doi.org/10.1029/2003GL018777
Description
Summary:[ 1 ] We use a global couple d atm osphere-ocean sea-ice model of interm ediate complexity to demonstrate that wind- forcing i s a crucial element to sustain meridional overturning flow i n t he Atlantic. Neglecting wind-stress in our multi- century-lon g simulations leads to a complete shutdown of the conveyor belt ci r culation. This r esult may have tremendous impacts f or an assessment of the sensitivity of 2-d clima t e models which typicall y do not capture wind-driven gyres. It is argued that wind effects may be a key element in determining the f ate and length of a collapsed THC state. Possible paleo implications will be discussed