Fig. 6: Insolation and sea surface temperature changes.
From: The response of AUSM to precession forcing and its relation to EASM and EAWM
Composite maps of (a, b) SOLIN and (c, f) sea surface temperature (SST) anomalies in March (a, c) and October (b, d). The composite anomalies are the differences between low and high precession states. Only those values above 95% confidence level are shown.
