Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/981
AuthorsLatif, M. 
TitleTropical Pacific influences on the North Atlantic Thermohaline Circulation
Issue Date2003
Series/Report no.46 (1)
URIhttp://hdl.handle.net/2122/981
Keywordsthermohaline circulation
air-sea
Subject Classification01. Atmosphere::01.01. Atmosphere::01.01.02. Climate 
03. Hydrosphere::03.03. Physical::03.03.02. General circulation 
AbstractMost global climate models simulate a weakening of the North Atlantic Thermohaline Circulation (THC) in response to enhanced greenhouse warming. Both surface warming and freshening in high latitudes, the so-called sinking region, contribute to the weakening of the THC. Some models simulate even a complete breakdown of the THC at sufficiently strong forcing. Here results from a state-of-the-art global climate model are presented that does not simulate a weakening of the THC in response to greenhouse warming. Large-scale air-sea interactions in the tropics, similar to those operating during present-day El Niños, lead to anomalously high salinities in the tropical Atlantic. These are advected into the sinking region, thereby increasing the surface density and compensating the effects of the local warming and freshening. The results of the model study are corroborated by the analysis of observations.
Appears in Collections:Annals of Geophysics

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