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Progress in Earth and Planetary Science
Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

From: Diurnal cycle over a coastal area of the Maritime Continent as derived by special networked soundings over Jakarta during HARIMAU2010

Fig. 5

Diurnal composite of precipitation and clouds, expressed by a spatial coverage of the infrared brightness temperature (TB(IR)) less than 230 K (black) and 270 K (gray), b the averaged TB(IR), c the rain rate from the TRMM 3B42, d the rain rate from the Serpong C-band radar, and e the vertical profile of the spatial coverage of the Serpong C-band radar echo with > 20 dBZ. All parameters are calculated within the area of the sounding array as in Fig. 1

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