Fig. 2: SSTAs regressed against inverse SAMI during DJF.
From: Role of Antarctic ozone in shaping East Asian summer precipitation variability
Regression of (A) 10 m wind anomalies (green vectors; m/s) and SLP anomalies (shadings; hPa) during DJF, SSTAs during (B) DJF, (C) MAM and (D) JJA on the inverse SAMI during DJF (shadings; K). Black stippling represents significance above the 90% confidence level. SWIO index is defined based on the red rectangular region.
