Geo-trekking in Ethiopia's Tropical Mountains: The Dogu'a Tembien District — illustration 1, PDF page 244
Source record
- Source
- Habesha History book corpus — Geo-trekking in Ethiopia's Tropical Mountains: The Dogu'a Tembien District
- Book
- Geo-trekking in Ethiopia's Tropical Mountains: The Dogu'a Tembien District
- Source reference
- Geo-trekking in Ethiopia's Tropical Mountains: The Dogu'a Tembien District; PDF page 244; embedded illustration 1, exact source rectangle 82.09, 62.36, 337.68, 254.04
- Page
- 244
- Publication year
- 2019
- Type
- Book illustration
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Source-page captions
Photo 14.4 Runoff transmission losses due to percolation typically occurs through the fractures (joints) in the limestone. May Anbesa sub-catchment. Photo Amanuel Zenebe (August 2012)
Fig. 14.6 Conceptual model of the average runoff response (runoff coefficient, RC%) of the rivers in Giba catchment through time (after Etefa et al. 2019). The start and two final points of the curve are based on detailed modelling outcomes. The scenario without SWC (soil and water conservation) and the modelled RC% of 1935–1936 were used to represent a ‘business-as-usual’ trend. Starting from the 1990s, this trend has been curbed by the introduction of SWC structures to reach the actual situation
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