Collective Role of Thermocline and Zonal Advective Feedbacks in the ENSO Mode*

The vertical advection of anomalous subsurface temperature by the mean upwelling and the zonal advection of mean sea surface temperature (SST) by anomalous current are known to be essential for the equatorial SST anomaly associated with the El Nin o-Southern Oscillation (ENSO). In the coupled model,... View More