Fig. 3From: Regional variation of the influence of cross-equatorial northerly surge towards diurnal cycle of rainfall over Java IslandHovmöller diagram of the hourly rainfall [shaded; mm h−1] and the meridional component of surface wind during [solid contour for southerly; dashed contour for northerly; m s−1) for a, e, i nonCENS, b, f, j CENS, and c, g, k the difference between CENS and nonCENS for a–c WJ region, e–g CJ region, and i–k EJ region. The topography feature of WJ, CJ, and EJ are shown in panels (d, h, and l), respectivelyBack to article page