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Young-Kwon Lim, Robin M. Kovach, Steven Pawson, and Guillaume Vernieres

structures also reveals that the 2015/16 El Niño is the strongest around the Niño-3.4 region (e.g., see Figs. 2 , 4 , 6 , and 7 ) but that the 1997/98 is the overall strongest event when assessed by conditions over the EP, the westerly wind burst (WWB) ( McPhaden et al. 1988 ; Kerr 1999 ; McGregor et al. 2016 ), subsurface water temperature, and anomalies in the thermocline depth. Another aspect of interest about the 2015/16 event is the relationship between the early onset of the 2015/16 event and

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