“…The most prolonged MHW of the past 70 years, occurring during 2013–2015, covered a broad region of the Northeast Pacific, with local maximum warming of 2.8°C (Bond et al., 2015; Di Lorenzo & Mantua, 2016), and did not end until after the development in the tropics of a strong El Niño. Its ecosystem impacts were unprecedented, including massive stranding, entanglement, and mortality of marine species and seabirds (Cavole et al., 2016; Jones et al., 2018; Santora et al., 2020) and prolonged harmful algal blooms that closed major fisheries (McCabe et al., 2016; Ryan et al., 2017; Sanford et al., 2019). This record‐breaking event led to enhanced scrutiny of many Northeast Pacific MHW aspects (Frolicher & Laufkotter, 2018; Holbrook et al., 2020), including their severities (Hobday et al., 2016; Jacox et al., 2020; Scannell et al., 2016), tropical and extratropical driving mechanisms (D. J. Amaya et al., 2020; Bond et al., 2015; Di Lorenzo & Mantua, 2016; Holbrook et al., 2019), and predictability (Hu et al., 2017; Jacox et al.…”