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

Figure 10

Composite anomaly distribution fields for the air temperature (°C) at 300 hPa level (brown contour) and 200 hPa level zonal components of the wind pattern in ms⁻¹ (black contour) at both (a) and (b); 700 hPa stream function (1 × 10⁶·kgs⁻¹) at (c, d) during anomalous (a, c) and (b, d) during suppressed periods of HREs. The shading (from a–d) denotes significant areas at 95% confidence interval.

(a)

(b)

(c)

(d)