On 26-29 June 2021, an unprecedented heatwave affected the Pacific Northwest (PNW) of the United States and western Canada. Temperature records were shattered, with all-time highs of 116°F (47°C) in Portland, Oregon, 108°F (42°C) in Seattle, Washington, and 121°F (49°C) in Lytton, British Columbia (Di Liberto, 2021). Heatwaves, characterized by prolonged periods of excessive heat, can have dangerous impacts on human health, infrastructure, and the environment (Campbell et al., 2018;McEvoy et al., 2009;Perkins-Kirkpatrick & Alexander, 2013;Ruffault et al., 2020), and the PNW heatwave was no exception. Over 500 deaths were attributed to the heatwave (Popovich & Choi-Schagrin, 2021), and the environment and infrastructure throughout the affected region were strained and damaged, with crops ruined and roads buckled due to the excessively hot temperatures (Baker & Sergio, 2021). The devastating and large-scale impacts of the PNW heatwave were exacerbated by the lack of adaptability of a region unaccustomed to such extreme high temperatures, with the observational record suggesting that this was a highly anomalous event (Figure 1).The meteorological conditions of the PNW heatwave were similar to previous deadly heatwaves in Europe and Russia (Black et al., 2004;Dole et al., 2011). These events are associated with atmospheric blocking patterns, which are known to cause extreme heatwaves (