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 7
The 850 hPa composite anomaly fields of the moisture flux (vectors) and its divergence (shading) during (a) anomalous HREs and (b) suppressed HREs, where positive and negative shading represents divergence and convergence, respectively. The scale vector corresponds to moisture flux 0.2 g/kg·m/s, and the moisture flux divergence contour interval is 0.2 × 10−8 g/kg/s.
| (a) |
| (b) |