Fig. 5: The spatial patterns of snow dynamics responses to the FCC in November.
From: Boreal forest cover change since 2000 contributes to cold winters in Eurasia
The anomalies of the a snow fall from atmosphere (mm of snow water equivalent), b snow cover (%), c snow persistence (day) as the consecutive length with snow cover on the ground, d surface albedo (%), and e snow-albedo feedback (%/ °C). Black dots indicate that the difference passes the significance test at a 95% confidence level.
