Fig. 5: Impacts of excessive light rain over EIO on south Asian summer monsoon circulation. | npj Climate and Atmospheric Science

Fig. 5: Impacts of excessive light rain over EIO on south Asian summer monsoon circulation.

From: Excessive equatorial light rain causes modeling dry bias of Indian summer monsoon rainfall

Fig. 5

a The difference in zonal-mean vertical circulation (with vertical velocity amplified 1000 times, vectors) and vertical velocity (without amplified, color shading) between U60 km and U3 km, averaged from 11th June to 9th July in 2020. b The difference in horizontal wind field (vectors) and geopotential height (color shading) at 850 hPa, averaged from 11th June to 9th July in 2020.

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