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The ToE is determined for the E-index and C-index, separately. The presence of the two ENSO regimes is underpinned by a non-linear Bjerknes feedback; specifically, zonal winds respond non-linearly to warm SST anomalies after large warm anomalies establish atmospheric deep convection in the equatorial eastern-Pacific, in turn, conducive to further SST warming by promoting the oceanic zonal advection, Ekman pumping, and thermocline feedback, constituting a positive feedback loop 35 , The potential to narrow uncertainty in regional climate predictions. Article Google Scholar Yeh, S. You can manage your subscription anytime via our Customer Portal.