Skip to main content

Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 5 | Geoscience Letters

Fig. 5

From: Regional variation of the influence of cross-equatorial northerly surge towards diurnal cycle of rainfall over Java Island

Fig. 5

Hourly evolution of a–f, m–r rainfall [shaded; mm h−1] and g–l, s–x overlayed vertically integrated moisture flux convergence (VIMFC) from 1000 to 850 hPa (shaded; mm) with surface wind convergence [red contour; s−1] and surface wind [vector; m s−1] from 13 to 04 LT with 3 h interval during nonCENS and CENS, respectively. The solid green contour is convergence and the dashed dark green contour is divergence. The brown arrow indicates the actual wind, while the black arrow indicates the diurnal component of the surface wind. The hatched areas indicate the rainfall difference during CENS and nonCENS satisfies 95% confidence levels of the statistical significance test

Back to article page