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

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The first step when per<strong>for</strong>m<strong>in</strong>g the quality assessment of our <strong>in</strong>terpolated DEMs was tocompare derived contours from the three different resolutions with the orig<strong>in</strong>al contours.As can be seen <strong>in</strong> Figure 5.5 the degree of agreement, regard<strong>in</strong>g terra<strong>in</strong> structure,<strong>in</strong>creases with <strong>in</strong>creased resolution.(a) (b) (c)Figure 5.5 Derived contours from DEMs <strong>in</strong> different resolutions. a) 100 meters, b) 30 meters andc) 10 meters. Red l<strong>in</strong>es represent<strong>in</strong>g orig<strong>in</strong>al contours and black l<strong>in</strong>es the derived contours fromthe <strong>in</strong>terpolated DEM.The second step <strong>in</strong> the quality assessment was to visually <strong>in</strong>spect shaded relief images ofthe <strong>in</strong>terpolated DEMs. This step made it possible to locate a number of anomalies thatshowed up as very contrast<strong>in</strong>g areas. It was possible to detect both geometricaldisplacement and attribute errors. An example of geometrical displacement is verticaledge errors, which can be seen <strong>in</strong> Figure 5.6 below. These errors were edited bycorrect<strong>in</strong>g the attribute table and the <strong>in</strong>terpolation repeated until a satisfy<strong>in</strong>g result wasobta<strong>in</strong>ed. A certa<strong>in</strong> degree of terrac<strong>in</strong>g can also be noticed along the slopes <strong>in</strong> the figure.(a)Figure 5.6 Shaded relief of DEM with 10-meter resolution. a) Show<strong>in</strong>g digitised errors lead<strong>in</strong>g tovertical edge error problems and (b) same area after edit<strong>in</strong>g of <strong>in</strong>put data.(b)50

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