Fig. 3: UV700 and rainfall anomalies for TC days with positive and negative SCRI, as well as their difference. | npj Climate and Atmospheric Science

Fig. 3: UV700 and rainfall anomalies for TC days with positive and negative SCRI, as well as their difference.

From: Tropical cyclones over the South China Sea suppress the monsoonal rainfall in southern China

Fig. 3: UV700 and rainfall anomalies for TC days with positive and negative SCRI, as well as their difference.

Composite 700-hPa horizontal wind (vectors; m s−1) and rainfall anomalies (mm day−1) for TC days with a positive and b negative SCRI. c is the difference between (a and b). Only vectors significant at the 95% confidence level are shown and shading significant at the 95% confidence level is stippled as red. Black shading represents mountains higher than 3000 m.

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