Over the last two decades, unusual warm events have been observed in the global ocean, significantly affecting our environment and society (Frölicher & Laufkötter, 2018). A marine heatwave (MHW) is commonly defined as a "prolonged discrete anomalously warm water event that can be described by its duration, intensity, rate of evolution, and spatial extent" (Hobday et al., 2016). Thus far, understanding and monitoring MHWs have received substantial scientific and public attention (Holbrook et al., 2019(Holbrook et al., , 2020Oliver et al., 2021). Recently, the most severe MHWs were attributed to anthropogenic climate change (Laufkötter et al., 2020), highlighting the necessity for motivated efforts to limit global warming. In the North Pacific, the largest MHW ever recorded, dubbed the Warm Blob, occurred between 2013 and 2015 with maximum sea surface temperatures that reached 6°C above average in some areas along the coast of Southern California (Bond et al., 2015). Impacts on marine ecosystems include harmful algal blooms, shifts in species range, and even local extinctions (Smale et al., 2019). Consequences have also been reported in the economic sector, since aquaculture and important fisheries are vulnerable to MHW events. For example, both commercial and recreational fisheries faced major challenges and loss of millions of dollars after the 2013-2015 northeast Pacific MHW (Cavole et al., 2016). Furthermore, the largest ever-recorded harmful algal bloom in the region, caused by the extreme temperatures, produced toxins that contaminated valuable shellfish and crab fisheries (McCabe et al., 2016). Increasing sea surface temperatures may also impact regional weather by affecting storms, precipitation, air temperature and droughts, the latter posing risks for potential wildfire events (Chikamoto et al., 2017). For example, anomalously high ocean temperatures in the northeast Pacific was the key forcing for the extensive dry winters in California during 2011-2014