“…Sea surface temperatures (SSTs) in the equatorial Pacific associated with El Niño-Southern Oscillation (ENSO) exert significant control over the interannual variability of the basin climate (e.g., Alexander et al, 2002;Harrison & Larkin, 1998;McPhaden et al, 2006), which drives major societal and economic impacts (e.g., Adams et al, 1999;Berry & Okulicz-Kozaryn, 2008;Cashin et al, 2017;Fisman et al, 2016). To first order, ENSO can be thought of as a collection of modes that are amplified along the zonal equatorial plane by positive coupled feedbacks between the ocean and atmosphere (Bjerknes, 1969;Jin, 1997;Suarez & Schopf, 1988).…”