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A simple dynamic model is proposed to illustrate the multidecadal oscillation of the AMOC. The proposed oscillation relies on alternating actions of positive and negative feedbacks, which are operated by a slow adjustment of the ocean circulation and the associated time delay in the advective flux response to meridional density gradient perturbation.
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This page is a summary of: Delayed Advective Oscillation of the Atlantic Thermohaline Circulation, Journal of Climate, March 2010, American Meteorological Society,
DOI: 10.1175/2009jcli3339.1.
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