The El Niño-Southern Oscillation (ENSO) is the most energetic air-sea coupled process on interannual time scales and profoundly impacts the global climate. ENSO is characterized by an irregular (2-7 years) oscillation of warm and cold sea surface temperature (SST) anomalies over the eastern and central equatorial Pacific. During the ENSO warm phase (El Niño), the tropical Pacific Ocean (TPO) and overlying atmosphere couple through the Bjerknes feedback mechanism (Bjerknes, 1969). The weakening of the zonal (i.e., east-west) SST gradient over the equatorial Pacific weakens the tropical easterly trade winds, further weakening the zonal SST gradient. However, this positive feedback cannot describe the turnabout of El Nino and its transition to the La Niña (ENSO cold phase). To explain the dynamics of the ENSO cycle, Wyrtki (1975, 1985 developed the "buildup and draining" hypothesis. According to this hypothesis, the excessively strong easterly trade winds build up warm water in the western equatorial