Fig. 1: Frequency of ROS (days per year).
From: Northern Pacific sea-level pressure controls rain-on-snow in North America

a During full water year and (b–d) seasons and (e) their variability with respect to elevation from mean sea level.
From: Northern Pacific sea-level pressure controls rain-on-snow in North America

a During full water year and (b–d) seasons and (e) their variability with respect to elevation from mean sea level.