Fig. 4: Simulated meridional circulation and surface temperature anomalies induced by SWIO SSTAs during boreal spring. | npj Climate and Atmospheric Science

Fig. 4: Simulated meridional circulation and surface temperature anomalies induced by SWIO SSTAs during boreal spring.

From: Role of Antarctic ozone in shaping East Asian summer precipitation variability

Fig. 4

Differences in (A) vertical velocity (shadings; 10–3 Pa/s) and meridional circulation (purple arrows) averaged over 60°–120°E and (B) surface temperature (shadings; K) between the SST_SWIO and SST_Clim experiments. Black stippling and purple arrows represent significance above the 90% confidence level.

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