Extended Data Fig. 5: Somali Jet response to changes in regional paleogeography.
From: Neogene South Asian monsoon rainfall and wind histories diverged due to topographic effects
Low level winds (850 hPa) during boreal summer (JJA) for a) late Miocene (LM) with low CO2 (LM-CO2); b) LM with Expanded Antarctic Ice Sheet (LM-AIS); c) LM with half present-day Anatolia-Iran topography (LM-NoAIO); d) LM with reduced topography in East African Highlands (LM-noEAHR); e) EM with uplifted East African Highlands (EM-EAH); f) EM with fully uplifted HTP region (EM-HTP) and g) EM with higher than present-day Himalaya orography (EM-Him).
