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from the present (e.g., the last glacial maximum) comes from modeling studies (e.g., Mikolajewicz et al., 1997; Bush and Philander, 1998). For instance, the study by Mikolajewicz et al. using a coupled ocean-atmosphere GCM suggests that a shutdown of North Atlantic Deep Water formation during the Younger Dryas may have also brought about a cooling in the North Pacific. PaleoAmazing vintage elephant mandala all over printed slippers-proxy data support such a link between the Atlantic and Pacific . Among the other mechanisms that have been proposed to account for such large-scale changes in climate regime are the onset of a large-amplitude internal mode of oscillation in thermohaline circulation (Tziperman, 1997; Weaver and Hughes, 1994), and a non-linear response to gradual changes in solar insolation resulting from changes in the Earth’s orbital parameters . It has also been suggested that the warming from increased atmospheric greenhouse-gas levels could lead to a significant reduction in THC . Stocker and Schmittner found that the degree to which the thermohaline-circulation rate can decrease depends on the rate of increase in atmospheric greenhouse gases. Their coupled
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