The 1960-1991 monthly mean FSU (Florida State University)wind stress data are decomposed into a vortical and a divergent component with each of which to force the model ocean in the context of a two-layer tropical Pac...The 1960-1991 monthly mean FSU (Florida State University)wind stress data are decomposed into a vortical and a divergent component with each of which to force the model ocean in the context of a two-layer tropical Pacific model.Evidence suggests that for the seasonal variation the ocean forcing does not produce a realistic cold tongue using either of the components and the tongue will not be effectively improved in its intensity and pattern even if the components are doubled or halved:the utilization of climatic mean wind stress(no decomposition is done of the wind stress)that contains its seasonal variation will lead to a realistic SST distribution on which is imposed,separately,the interannual anomalies of each of the components so as to get the SSTA pattern:under the action of the interannual anomaly of the vortical(divergent)component there arises qnite intense SSTA oscillation marked by noticeable ENSO periods(feeble SSTA with higher oscillation frequency for obscure ENSO periods),thereby illustrating that the roles of the two components differ from each other in the genesis of SST variation on a seasonal and an interannual basis such that a realistic cold tongue pattern follows under the joint effects on the model ocean of the two components of wind stress while rational E1 Nino/La Nina phenomena result under the forcing of an anomalous wind stress vortical component.Moreover,the divergent component is innegligible in generating a mean climatic condition of the ocean sector but of less importance compared to the vortical component in ENSO development.展开更多
基金The work is supported jointly by the National Natural Science Foundation of China (Grant 19775265)Research Starting Funds for Returned Scientific Personnel under the PRC Education Commission.
文摘The 1960-1991 monthly mean FSU (Florida State University)wind stress data are decomposed into a vortical and a divergent component with each of which to force the model ocean in the context of a two-layer tropical Pacific model.Evidence suggests that for the seasonal variation the ocean forcing does not produce a realistic cold tongue using either of the components and the tongue will not be effectively improved in its intensity and pattern even if the components are doubled or halved:the utilization of climatic mean wind stress(no decomposition is done of the wind stress)that contains its seasonal variation will lead to a realistic SST distribution on which is imposed,separately,the interannual anomalies of each of the components so as to get the SSTA pattern:under the action of the interannual anomaly of the vortical(divergent)component there arises qnite intense SSTA oscillation marked by noticeable ENSO periods(feeble SSTA with higher oscillation frequency for obscure ENSO periods),thereby illustrating that the roles of the two components differ from each other in the genesis of SST variation on a seasonal and an interannual basis such that a realistic cold tongue pattern follows under the joint effects on the model ocean of the two components of wind stress while rational E1 Nino/La Nina phenomena result under the forcing of an anomalous wind stress vortical component.Moreover,the divergent component is innegligible in generating a mean climatic condition of the ocean sector but of less importance compared to the vortical component in ENSO development.
