Fig. 5: Seasonal cycles of insolation and monsoon precipitation.
From: The response of AUSM to precession forcing and its relation to EASM and EAWM
Composite seasonal cycles of insolation at top of atmosphere anomalies (a, b) and precipitation anomalies in monsoon regions (c). The composite anomalies are differences between low and high precession stages. (a) shows the related local insolation for EAM (30°N-40°N) and for AUM (15°S-5°S). (b) shows the related remote insolation for EAM (45°N-60°N) and for AUM (60°S-30°S).
