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6. DATABASE CONSTRAINTS<br />

The greatest problem was the lack of georeferenced aerial photographs for the area. Google<br />

Earth was investigated to determine if it would provide value to the project, but the quality of<br />

the images was too poor for the purpose of this project. The 1:50 000 aerial photographs, as<br />

obtained from the Chief Directorate: Surveys and Mapping at the Department of Land<br />

Affairs, Mowbray, Cape Town, was the only complete set of aerial photographs available<br />

for the site. The georeferencing of these aerial photographs was based on the 1:50 000<br />

topographical map and accuracy is therefore dependant on the accuracy of the topographical<br />

layers. In addition, all aerial photographs are skewed towards the edges due to the concave<br />

structure of the camera lens. We attempted to correct this feature during the georeferencing<br />

process, but the effect could not be removed completely. The <strong>wetland</strong>s located to the edges<br />

of the aerial photographs may therefore be slightly removed from their exact position.<br />

Where areas under cultivation were obviously located on a seepage area the <strong>wetland</strong> was<br />

indicated and the status of the <strong>wetland</strong> was given as E or F (destroyed). Some additional<br />

seepage areas covered by cultivation may occur, but have not been identified. This is<br />

because <strong>wetland</strong>s under cultivation are not easily distinguished. Patchiness in a cultivated<br />

area can be caused by a number of influences, including differences in soil and patchy<br />

distribution of fertiliser, in addition to the presence of seepage <strong>wetland</strong>s. Other highly<br />

disturbed <strong>wetland</strong>s may also not be identifiable on the aerial photographs as <strong>wetland</strong>s and<br />

these <strong>wetland</strong>s will be absent from the <strong>wetland</strong> layer. In addition, small <strong>wetland</strong>s are not<br />

visible on the 1:50 000 aerial photographs and are therefore not included.<br />

Tonal variations between the aerial photographs complicated the mapping of the <strong>wetland</strong>s on<br />

the aerial photographs. The changes from one strip of aerial photographs to another may be<br />

due to the time of day the photographs were taken and the light quality. Even without cloud<br />

cover the light quality may differ from day to day.<br />

7. COMPARISON TO THE NATIONAL LANDCOVER WETLAND LAYER<br />

The final Landcover <strong>wetland</strong> layer, completed in June 2006, was compared to the completed<br />

UORC <strong>wetland</strong> database. The Landcover <strong>wetland</strong> layer compared very well to the UORC<br />

<strong>wetland</strong> database, since all of the Landcover <strong>wetland</strong>s were already identified in the UORC<br />

database (Figure 20).<br />

Wetland Database for UORC - 89 -

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