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Finding Potential Sites for Small-Scale Hydro Power in Uganda: a ...

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To evaluate accuracy of the absolute elevation of the DEMs, we calculated the RMS-at four different reference locations. The result, which can be seen <strong>in</strong> Table 5.1errorsshows that the lowest RMS-errors occurs at steep areas <strong>in</strong> the DEM with 10-meterresolution. At flat areas the RMS-error are with<strong>in</strong> the same range of values, regardless ofresolution. There is a noticeable <strong>in</strong>crease <strong>in</strong> RMS-error with <strong>in</strong>creased cell-size <strong>in</strong> steepareas.Table 5.1 RMS-error <strong>for</strong> the DEM at the references l<strong>in</strong>es, <strong>in</strong> three different resolutions.Resolution Flat 1 Flat 2 Steep 1 Steep 2 Mean RMS100 meter 14.64488 14.32897 29.07937 43.40787 25.3652730 meter 12.84792 14.78252 16.47471 23.72902 16.9585410 meter 12.83892 15.45371 7.22123 7.36828 10.72054The outcome of the quality assessment po<strong>in</strong>ts to that the 10-meter resolution DEM is agood choice <strong>for</strong> our analysis. It has the highest degree of accuracy regard<strong>in</strong>g both terra<strong>in</strong>structure and absolute elevation. Figure 5.7 shows the digital elevation model over ourstudy area.Figure 5.7 A 3-D image of the DEM with 10-meter resolution over the districts Kisoro and Kabale.A five-time vertical exaggeration factor has been used to highlight the shapes of the landscape.Lighter areas represent high elevation and darker low.5.2.2 AlgorithmThe first unprocessed output data, <strong>for</strong> the entire study area, is produced by the algorithmwith<strong>in</strong> a couple of m<strong>in</strong>utes. A selection from the output data can be seen <strong>in</strong> Figure 5.8a.A first look at the output gives a rather vague impression of what the result actuallyrepresent, but when apply<strong>in</strong>g the contours (see Figure 5.8b) the potential sites appear51

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