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Environmental and Social Impact Assessment - Gibe III

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<strong>Gibe</strong> <strong>III</strong> – <strong>Environmental</strong> <strong>and</strong> <strong>Social</strong> <strong>Impact</strong> <strong>Assessment</strong> 300 ENV R CS 002 C - A9003099<br />

2 13 3<br />

• Hydrological studies for other regions comprised in the catchment of interest<br />

• <strong>Gibe</strong> <strong>III</strong> Hydrological Study of the Basic Design 3 .<br />

The transformation of rainfall into runoff has been carried out developing a hydrological model of the whole<br />

watershed by means of HEC HMS 3.1.0 software in order to better control the process of formation of the<br />

flood over the contributing catchments taking into account the routing effect due to the operating upstream<br />

<strong>Gibe</strong> I Dam, the routing effect along the river, <strong>and</strong> the hydrographs combination in correspondence of the<br />

junctions.<br />

Geomorphologic parameters of the single catchment have been derived from a digital terrain model using<br />

GIS tool.<br />

Rainfall analysis<br />

Daily precipitation records have been used to generate 3-, 5-, 7-, 10- <strong>and</strong> 15-day records.<br />

The longest duration of 15 days has been preliminarily chosen as the critical storm duration basing on<br />

experience of catchments of comparable extension (about 35,000 km 2 ) <strong>and</strong> basing on some empirical<br />

expression 2 such as dcrit = (A/100 + 0.5) 0.5 , which provides 18 days for the given area.<br />

Rainfall-runoff analysis for longer durations adopting extrapolated data has shown, indeed, that peak flood<br />

increase after 15 days is practically negligible.<br />

Frequency analysis of extreme precipitation<br />

A brief analysis of the mean of the annual max records shows that this value varies in a narrow range 61.5<br />

mm – 49.2 mm if Gedo with 28.7 mm is excluded. This is likely due to the comparable altitude of the<br />

stations.<br />

Gedo station is located just outside of the <strong>Gibe</strong> <strong>III</strong> catchment <strong>and</strong> its point precipitation is strongly affected<br />

by the highl<strong>and</strong> which bounds the basin. Moreover Gedo is not only out of the boundary but also very close<br />

to Ejaji station, therefore as specified later on, its areal weight in the hydrological elaborations is very<br />

modest.<br />

Consequently all the stations have been considered in the frequency analysis.<br />

A “regional” approach, based on the assumption of the hydrological homogeneity of the sites in the <strong>Gibe</strong> <strong>III</strong><br />

catchment area, has been applied. This approach is considered since no large number of records is available<br />

while a long dataset is m<strong>and</strong>atory for a high return period analysis in a homogeneous region. The method<br />

assumes that the probability distribution of rainfall at different sites within a region is the same except for a<br />

scale parameter, also known as “index storm”, which reflects the rainfall characteristics of the particular site<br />

<strong>and</strong> is usually assumed to be the mean rainfall at the station.<br />

The following table lists the main results 14 of the statistical elaborations for 100-, 1,000- <strong>and</strong> 10,000-year<br />

frequencies.<br />

13<br />

EEPCO, “Gilgel <strong>Gibe</strong> Hydroelectrical Project, Feasibility Study Main Report”, ELC Electroconsult - ENEL, Feb<br />

1998<br />

14<br />

300 HYD R SP 001 EXTREME FLOODS REPORT Jun 07 lc, studio pietrangeli, rome<br />

CESI SpA - Mid-Day International Consulting Engineers Page 108

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