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The Impacts of Topography on Spatial and Temporal Rainfall Distribution over Rwanda Based on WRF Model

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Figure

Figure 1. Three model domains used in the study (a) topography elevation (m) and location of Rwandan provinces (c)
Table 2. High altitude regions in the north and western provinces of Rwanda.
Figure 3. The accumulated rainfall (mm) for WRF with actual topography (AT) (a), (d), WRF with reduced topography (RT) (b), (e) and difference between actual and reduced topography (AT-RT) (c), (f) for the period from April 7 to 9 and October 29 to 31, 201
Figure 4. The mean moisture flux over the period 7 to 9 April and 29 to 31 October 2012 at 800 hpa (a), (c) with actual topography (AT), (b), (d) re-duced topography (RT) respectively
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