Extended Data Fig. 9: Moisture transport response to change in regional physiography.
From: Neogene South Asian monsoon rainfall and wind histories diverged due to topographic effects
Late summer vertically integrated moisture transport (JJA) a) late Miocene (LM); b) LM-NoAIO; c) LM-NoEAP, d) early Miocene (EM). Change in vertically integrated moisture transport (JJA) in response to e) change in Anatolia-Iran topography (LM-NoAIO vs. LM); f) emersion of the Eastern Arabian Peninsula (LM-NoEAP vs. LM-NoAIO) and g) paleogeographic evolution between the early and the late Miocene (LM vs. EM).
