Tropical Pacific influences on the North Atlantic Thermohaline Circulation

Most 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...

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Bibliographic Details
Main Author: M. Latif
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2003-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3392
Description
Summary:Most 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.
ISSN:1593-5213
2037-416X