Fig. 1From: Seasonal modulation of the Asian summer monsoon between the Medieval Warm Period and Little Ice Age: a multi model studySeasonal variation of insolation (W m−2) at the top of the atmosphere averaged over 10 PMIP3 models. Shading represents the anomaly between the MWP (950–1250 A.D.) and LIA (1400–1800 A.D.; hereafter ML anomaly). Contours represent climatology in the LIABack to article page