Extended Data Fig. 3: Variance explained by grid point air-sea correlations.
From: Signature of the western boundary currents in local climate variability
The square of grid point correlation coefficients of (a, c, e, g) vertical motion anomalies at 850 hPa correlated with SST anomalies and (b, d, f, h) high-pass spatially filtered precipitation anomalies correlated with SST anomalies. See Methods for more details. Results are based on monthly mean ERA5.
