Fig. 2: Precipitation intensity spectrum during active monsoon in 2020. | npj Climate and Atmospheric Science

Fig. 2: Precipitation intensity spectrum during active monsoon in 2020.

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

Fig. 2

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. The spatial distribution of difference in light rainfall frequency between (b) U60 km and CMORPH; (c) U3 km and U60 km during the same period. The regions surrounded by red dotted line are same as that in Fig. 1.

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