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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 1 | Geoscience Letters

Fig. 1

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

Fig. 1

a–c ERA5 daily mean of surface wind [vector;ms−1] overlayed with the meridional wind [shaded; ms−1] and d–f daily mean of rainfall [shaded; mm day−1] of IMERG for a, d nonCENS, b, e CENS, c surface wind difference between CENS and nonCENS (CENS–nonCENS) and f daily rainfall of \(\frac{{{\text{CENS}} - {\text{nonCENS}}}}{{{\text{nonCENS}}}} \times 100{\text{\% }}\)[The positive (negative) value in the blue (red) is the enhancement (reduction) percentage of daily rainfall during CENS to nonCENS]. The hatched areas indicate the rainfall difference during CENS and nonCENS satisfies 95% confidence levels of the statistical significance test. The black rectangle indicates the used CENS index area in this study

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