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The authors examined the effect of oceanic baroclinicity and atmospheric cooling on the subduction in baroclinic ocean using three dimensional nonhydrostatic model. It turns out that stronger baroclin...icity causes larger subduction rate despite similar penetration speed of the depth to which subducted water is transported (subduction depth), while stronger cooling results in more rapid penetration speed of the subduction depth though it affects little on the subduction rate as long as cooling is imposed. These results suggests that both baroclinicity and cooling are important parameters for heat and material transports between the surface mixed layer and the interior baroclinic ocean and hence for decadal variations in climate systems.続きを見る
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