Figure 6: Climate anomaly associated with large projected decease in regional snowpack.
From: Large near-term projected snowpack loss over the western United States
Difference in winter (January, February and March) mean sea level pressure (contours in hPa) and surface air temperature anomalies (shading) between the five CanESM2 ensemble members with the lowest winter SWEmax averaged over 2030–2040 and the five ensemble members with the highest winter SWEmax averaged over the same period.
