The western United States (US) is a global snow drought hotspot (Huning & AghaKouchak, 2020b), and has experienced significant mountain snowpack declines (∼15%-30%) since the mid-1900s (Mote et al., 2018. In particular, the Cascade Range (Cascades) in the US Pacific Northwest (PNW) has undergone the most dramatic declines during the instrumental era (Mote et al., 2005(Mote et al., , 2018, with the largest climate sensitivities and reduced snowpack predictability (Livneh & Badger, 2020). Oregon has sustained the greatest reductions (Mote, 2003;Mote et al., 2005) and contains approximately half of "at-risk" Cascades snow (Nolin & Daly, 2006). Analysis of observational data sets dating to the mid-20th century suggest a 16% loss in Cascades snowpack independent of internal variability from 1930 to 2007 (Stoelinga et al., 2010).Oregon Cascade snowpacks act as natural reservoirs for water supply that are slowly released in the spring and summer months when demand is highest (Barnett et al., 2005;Siirila-Woodburn et al., 2021). Located adjacent to the state's largest human population centers, they supply up to 75% of annual societal, economic, agriculture, and ecosystem water demands (United States Department of Agriculture, Natural Resources Conservation Service, 2022). The potential impacts of snow drought (Harpold et al., 2017) in Oregon were brought into sharp focus during the 2014-2015 snow drought event (spanning the 2014 and 2015 water years) when near-average winter precipitation was accompanied by exceptionally warm temperatures, resulting in precipitation primarily falling as rain rather than snow (a "warm snow drought") (