The interdecadal change of the mean-state and two types of El Nino was investigated based on the analysis of observational data from 1980 to 2010. It was found that easterly trades and sea surface temperature (SST) gradients across the equatorial Pacific undergo a regime change in 1998/1999, with enhanced trades and a significant cooling (warming) over tropical eastern (western) Pacific in the later period. Accompanying this mea-state change is more frequent occurrence of central Pacific (CP) El Nino during 1999-2010. The diagnosis of air-sea feedback strength showed that atmospheric precipitation and wind responses to CP El Nino are greater than those to EP El Nino for given a unit SSTA forcing. The oceanic response to the same wind forcing, however, is greater in the EP El Nino than in the CP El Nino. A mixed-layer heat budget analysis reveals that zonal advection (thermocline change induced vertical advection) primarily contributes to the CP (EP) El Nino growth.
The role of the mean SST zonal gradient in El Nino selection was investigated through idealized numerical experiments. With the increase of the background zonal SST gradient, the anomalous wind and convection response to a specified EP or CP SST anomaly (SSTA) shift to the west. Such a difference results in a bifurcation of maximum SSTA tendency, as shown from a simple ocean model. The numerical results support the notion that a shift to the La Nino-like interdecadal mean state is responsible for more frequent occurrence of CP-type El Nino.
如有問題歡迎與系統管理員聯繫 
