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 13

A spatial distribution pattern of the (a) zonal wind anomaly fields in ms−1 and (b) horizontal wind divergence anomaly fields (contour intervals 0.2 × 10−6·s−1) at 200 hPa isobaric level during anomalous HREs based on 1980–2010 climatology.
(a)
(b)