Fig. 6: South Asian summer monsoon rainfall and circulation during active monsoon in 2020.
From: Excessive equatorial light rain causes modeling dry bias of Indian summer monsoon rainfall

a The difference in mean rainfall between V4 kmTropics and U60 km, averaged from 11th June to 9th July in 2020. b The horizontal wind field (vectors) and speed (color shading) at 850 hPa in V4 kmTropics, averaged from 11th June to 9th July in 2020. c The zonal-mean vertical circulation (with vertical velocity amplified 1000 times, vectors) and vertical velocity (without amplified, color shading) in V4 kmTropics, averaged from 11th June to 9th July in 2020.