%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Goelzer, H.
%A Mignot, Juliette
%A Levermann, A.
%A Rahmstorf, S.
%T Tropical versus high latitude freshwater influence on the Atlantic circulation
%D 2006
%L fdi:010037648
%G ENG
%J Climate Dynamics
%@ 0930-7575
%M CC:0002412582-0004
%N 7-8
%P 715-725
%R 10.1007/s00382-006-0161-5
%U https://www.documentation.ird.fr/hor/fdi:010037648
%> https://www.documentation.ird.fr/intranet/publi/2006/11/010037648.pdf
%V 27
%W Horizon (IRD)
%X We investigate the model sensitivity of the Atlantic meridional overturning circulation (AMOC) to anomalous freshwater flux in the tropical and northern Atlantic. Forcing in both locations leads to the same qualitative response: a positive freshwater anomaly induces a weakening of the AMOC and a negative freshwater anomaly strengthens the AMOC. Strong differences arise in the temporal characteristics and amplitude of the response. The advection of the tropical anomaly up to the deep water formation area leads to a time delayed response compared to a northern forcing. Thus, in its transient response, the AMOC is less sensitive to a constant anomalous freshwater flux in the tropics than in the north. This difference decreases with time and practically vanishes in equilibrium with constant freshwater forcing. The equilibrium response of the AMOC shows a non-linear dependence on freshwater forcing in both locations, with a stronger sensitivity to positive freshwater forcing. As a consequence, competitive forcing in both regions is balanced when the negative forcing is about 1.5 times larger than the positive forcing. The relaxation time of the AMOC after termination of a freshwater perturbation depends significantly on the AMOC strength itself. A strong overturning exhibits a faster relaxation to its unperturbed state. By means of a set of complementary experiments (pulse-perturbations, constant and stochastic forcing) we quantify these effects and discuss the corresponding time scales and physical processes.
%$ 032