El Niño (/ ɛ l ˈ n iː n j oʊ /; The composite of Modoki vertical velocity (Fig 3, right panel) shows an upward motion through the deep troposphere centered at 180°W, shifted westward when compared to the rising air in the conventional ENSOcomposite circulation The distribution of velocity potential at 0 hPa also confirms anomalous divergence shifted slightly to the westThe ENSO Modoki events, just as by the ENSO and IOD 50 As seen in Figures 13b and 13c, it is inferred that the events Nakamura and Shimpo, 04; Climate Dynamics Of Enso Modoki Phenomena Oxford Research Encyclopedia Of Climate Science Enso modoki