Fig. 4: Characteristics of surface and low-level climate changes.
From: The response of AUSM to precession forcing and its relation to EASM and EAWM
Composite maps of (a, d) moist static energy at 850 hPa (MSE850) and (b, e) surface temperature (TS, shading) along with sea level pressure (SLP, contour), and (c, f) SLP (shading) along with wind at 850 hPa (vector) anomalies in DJF (a–c) and JJA (d–f). The composite anomalies are the differences between low and high precession states. Only those values above 95% confidence level are shown. The results are derived from ORB run.
