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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

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

Fig. 3

Time–height cross sections of the sounding-derived parameters averaged over the array: a the zonal wind, b potential temperature anomaly, c moisture anomaly, d TB(IR), and e TRMM 3B42 rainrate are shown. All values are averaged over the array. Anomalies in b and c are from the average through the ASP at each pressure level. The vertical dashed black lines indicate the start and the end of the EASP. The MJO index by Wheeler and Hendon (2004) is shown on the top

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