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 11
(a) 600–300 hPa average layer temperature anomalies (contour interval 0.02°C) and (b) the difference in zonal wind anomalies between 600 and 300 hPa levels (contour interval 0.2 ms−1) during anomalous periods of HREs. Shading represents areas at 95% confidence level.
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