Research Article
Assessing Prone Areas to Heavy Rainfall and the Impaction of the Upper Warm Temperature Anomaly during March–May Rainfall Season in Tanzania
Figure 14
Composite spatial pattern for the 200 hPa vertical velocity anomaly (contour intervals 0.2 × 10−2·Pas−1) field during anomalous HREs based on 1980–2010 climatology. Negative values indicate upward motion, while shading represents significant areas at 95% confidence interval.