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He added that the industry's voluntary code barring most adverts before the watershed were not necessarily effective.
From the flow accumulation layer, the valley shapes in the watershed were obtained.
Drain spacings in different parts of the watershed were estimated from the watershed tile line map.
Six floodplain/channel sites, from high to low in the watershed, were selected for intensive study.
The SMAF analysis indicated soils within the watershed were functioning at 87% of their full potential.
The linear morphometric linear parameters of the watershed were calculated using standard formulae as given in Table 2.
Therefore, for watersheds with more than one valley, all valleys in the watershed were considered in the process.
Meteorological stations at Kofele, Shashemene, and Awassa, which are neighbor to the study watershed, were also considered in this study.
Morphometric parameters of the watershed were evaluated by computations of linear and areal aspect using standard methodology in GIS environment.
As many as 14 landscape indices – measuring the composition and configuration in each watershed – were calculated using Fragstats 3.3.
One urban and one forested watershed were selected for both validation and testing purposes, while 4 forested, 1 urban, and 1 pastoral watershed were used for training the model.
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