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Is the wind stress forcing essential for the meridional overturning circulation?
Author(s) -
Timmermann A.,
Goosse H.
Publication year - 2004
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2003gl018777
Subject(s) - wind stress , ocean gyre , forcing (mathematics) , shutdown of thermohaline circulation , climatology , thermohaline circulation , geology , environmental science , atmospheric sciences , north atlantic deep water , subtropics , fishery , biology
We use a global coupled atmosphere‐ocean sea‐ice model of intermediate complexity to demonstrate that wind‐forcing is a crucial element to sustain meridional overturning flow in the Atlantic. Neglecting wind‐stress in our multi‐century‐long simulations leads to a complete shutdown of the conveyor belt circulation. This result may have tremendous impacts for an assessment of the sensitivity of 2‐d climate models which typically do not capture wind‐driven gyres. It is argued that wind effects may be a key element in determining the fate and length of a collapsed THC state. Possible paleo implications will be discussed.