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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 />

Climate <strong>and</strong> rainfall features<br />

The climate is classifiable as tropical humid in the highl<strong>and</strong>s that include the areas surrounding Jima <strong>and</strong><br />

around the headwaters of the Gojeb River. For the rest, <strong>and</strong> greatest part, of the watershed the climate is<br />

classifiable as a tropical sub-humid, intermediate between the tropical humid <strong>and</strong> the hot arid climate<br />

characteristic of the southernmost part of the floodplain toward Lake Turkana. The seasonal variation in<br />

climate is associated with the oscillation of the Inter-Tropical Convergence Zone (ITCZ), a low pressure area<br />

of convergence. The ITCZ shifts during the year northwards across southern Ethiopia from September to<br />

November <strong>and</strong> southwards from March to May, giving origin to the alternation of a wet (from June to<br />

September) <strong>and</strong> a dry (from December to April) season. During the wet season the area is under the influence<br />

of Atlantic equatorial westerlies <strong>and</strong> southerly winds from the Indian Ocean, producing strong precipitation,<br />

mainly due to the Atlantic moist component. During the dry season the moist air comes from the Gulf of<br />

Aden <strong>and</strong> the Indian Ocean, causing little rains.<br />

As the main source of moist air is from the Atlantic Ocean, from the SW, the eastern parts of the highl<strong>and</strong>s<br />

are more or less rain shadowed. This effect can be seen on the isohyetal map of the area, reported in the Omo<br />

River Master Plan (Figure 5.4). The area of greatest rainfall is to the NW of Jima (outside the <strong>Gibe</strong> Basin).<br />

Rainfall declines sharply in the lower lying southern parts of the basin. According to the isohyetal map of the<br />

OGMP, the rainfall ranges from over 1900 mm/year in the northern <strong>and</strong> western part of the basin, to about<br />

1200 mm/year in the lower part of the project area. Rainfall rates decrease strongly southwards, to less than<br />

300 mm/year near Lake Turkana.<br />

Hydro-meteorological data<br />

The hydrological elaborations reported in the following sections are mainly based on rainfall <strong>and</strong> runoff data<br />

provided mainly by gauges of the Ethiopian National Meteorological Service Agency <strong>and</strong> Ethiopian Water<br />

Resources Authority. In addition external data were used coming only from officially approved documents<br />

related to other project in the same area. These documents are:<br />

1) the already mentioned “Omo-<strong>Gibe</strong> River Basin Integrated Development Master Plan Study”, Vol. VI -<br />

Water Resources Surveys <strong>and</strong> Inventories, Dec 1996, carried out by Richard Woodroofe & Associates<br />

for the Ministry of Water Resources of the Federal Democratic Republic of Ethiopia,<br />

2) the Gilgel <strong>Gibe</strong> Hydroelectric Project, Hydrological Report, Nov 1995, carried out by ELC<br />

Elettroconsult <strong>and</strong> ENEL SpA for the Ministry of Mines <strong>and</strong> Energy - Ethiopian Electric Light <strong>and</strong><br />

Power Authority,<br />

3) the Gojeb Medium Hydropower Project, Pre-Feasibility Study, Vol.1 - Executive Summary, Vol. 3 -<br />

Annex A, Hydrology, Oct 1996, carried out by Howard Humphreys, Coyne et Bellier, Rust Kennedy &<br />

Donkin,<br />

4) the Feasibility Study of Halele-Werabesa Stage II Hydropower Project, Main Report, Dec 2004, carried<br />

out by Lahmeyer International GmbH for the Ethiopian Electric Power Corporation.<br />

CESI SpA - Mid-Day International Consulting Engineers Page 97

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