Fig. 7From: Diurnal cycle over a coastal area of the Maritime Continent as derived by special networked soundings over Jakarta during HARIMAU2010Diurnal composite of the time–height cross section, for the zonal wind (a, d), meridional wind (b, d), and horizontal divergence (c, f); a to c are the composites of the absolute values, whereas d to f are the composites of the anomalies from the 1-day running mean at each pressure levelBack to article page