“…Evaporative demand ( E 0 )—the upper limit of actual evapotranspiration ( ET ) that could occur given unlimited surface water supply (Hobbins et al, 2017)—has a strong connection to drought and wildfire potential in the western United States (e.g., Abatzoglou & Kolden, 2013; Abatzoglou & Williams, 2016; Littell et al, 2016; McEvoy et al, 2016) and globally (e.g., Dai, 2011; Vicente‐Serrano et al, 2010). In California and Nevada, elevated E 0 contributed to the 2012–2016 drought's severity (Hobbins et al, 2016; McEvoy et al, 2016; Shukla et al, 2015; Williams et al, 2015) and to wildfire potential (Brown et al, 2020; McEvoy et al, 2019; Nauslar et al, 2019). Although E 0 is sometimes calculated from temperature alone, a physically based E 0 formulation is critical to obtaining realistic estimates that include not only temperature changes but also the wind speed, humidity, and incoming shortwave radiation components that drive land surface‐atmosphere interactions and drying (Hidalgo et al, 2005; Hobbins et al, 2017).…”