Extended Data Fig. 1: Paleogeographic reconstruction used in the reference simulations.
From: Neogene South Asian monsoon rainfall and wind histories diverged due to topographic effects
a) late Miocene (LM) and b) early Miocene (EM) simulations. Initial bathymetry is more detailed in LM than in EM paleogeography, but the model resolution (2° by 2°) mitigates the difference by smoothing small variations.
