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Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

From: Meridional march of diurnal rainfall over Jakarta, Indonesia, observed with a C-band Doppler radar: an overview of the HARIMAU2010 campaign

Fig. 4

Temporal variations of the sounding data obtained at Bogor. Time–height cross-sectional views of the sounding data obtained at Bogor during the campaign period. a Equivalent potential temperature (anomaly), b specific humidity (anomaly), and c zonal and d meridional wind speeds. Anomalies were calculated from the period averaged data of Bogor at each height

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