Atmospheric rivers (ARs) are long, narrow filaments of strong horizontal water vapor transport in the lower troposphere, typically associated with cold fronts of extratropical cyclones (Cordeira et al., 2013;Ralph et al., 2004Ralph et al., , 2017. ARs play an important role in the hydrological cycle, accomplishing most of the poleward moisture transport in the atmosphere at midlatitudes (Newman et al., 2012;Zhu & Newell, 1998). Landfalling ARs can be forced upwards by orography, leading to extreme precipitation and a range of hydrological impacts (Neiman et al., 2008). In California, for example, precipitation due to ARs has ended droughts and caused floods, landslides, and other debris flows (