Fig. 8From: Meridional march of diurnal rainfall over Jakarta, Indonesia, observed with a C-band Doppler radar: an overview of the HARIMAU2010 campaignDiurnal meridional variations of the CDR echo in each period. Same as Fig. 6b but 24-h views of DRMM averaged for the a CENS active, b transition, and c inactive periods, as well as the d whole periodsBack to article page