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Various important features could be found on the open ocean deep convection and the subsequent deep water formation from large
eddy simulation (LES), and the results were applied to the East Sea (Japan Sea). It was found that under a strong cold wind
outburst with the heat flux of 1000 Wm−2 for 5 days generates a deep convection which can penetrate to the depth 1500 m, but under the continuous cooling with the
heat flux of 250 Wm−2 the growth of a mixed layer is suppressed at 700 m. The effects of the spatial and temporal variations of the surface forcing
were investigated with regard to the penetrative depth of convection, the generation of baroclinic eddies, the volume of the
water mass formation, and the intensity of the rim current. The deep water formations in the intermediate and deep layer of
the East Sea were explained in terms of the simulation results, and the intensity of the consequent circulation and the volume
of water mass formation were compared with the observation data.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献