Fig. 6From: Regional variation of the influence of cross-equatorial northerly surge towards diurnal cycle of rainfall over Java IslandVertical cross section of daytime (10–16 LT) composite of virtual potential temperature (\(\theta_v\)) from ERA5 [contour; K] and meridional circulation [actual v-wind and w-wind (multiplied by 10); vector; m s−1] over a–c WJ, d–f CJ, and g–i EJ for a, d, g nonCENS, b, e, h CENS and c, f, i difference between CENS and nonCENS (CENS - nonCENS)Back to article page