Assessing Prone Areas to Heavy Rainfall and the Impaction of the Upper Warm Temperature Anomaly during March–May Rainfall Season in Tanzania

Figure 8

Composite velocity potential and wind divergent anomalies at (a) 850 hPa and (b) 200 hPa for stations over the northern coast and NEH during anomalous heavy rainfall; units for velocity potential being 1 × 10⁶·m²s⁻¹; divergent wind (s⁻¹) while the shading indicates significant areas at 95% confidence interval.

(a)

(b)