Fig. 5: Atmospheric circulation response in the CESM simulation.
From: A dynamic link between spring Arctic sea ice and the Tibetan Plateau snow increment indicator
Response of a OND, b DJF and c FMA wave activity flux (vectors; unit: W m−2) and geopotential height (shadings; unit: gpm) anomalies at 250-hPa to the TP albedo forcing obtained by the difference response between the high albedo and control experiments. The stippled regions indicate the statistical significance of the geopotential height anomalies at the 5% level.
