Fig. 4: Frequency, accumulated amount and latent heat of precipitation with different intensity levels over the EIO during active monsoon.
From: Excessive equatorial light rain causes modeling dry bias of Indian summer monsoon rainfall

a the frequency of five rainfall intensity levels in CMORPH, GPM, U60 km and U3 km, counted from 11th June to 9th July in 2020 over the EIO (50–100oE, 0–10oS). b The accumulated rainfall of rainfall with different intensities. c The column-averaged latent heat released by rainfall with different intensities in U60 km and U3 km. d The contribution (frequency times column-averaged latent heat with the same level) to averaged latent heat by rainfall with different intensities in U60 km and U3 km.