Course Title: Geography of Ethiopia and the Horn
Instructor: Belete Ejigu (PhD), Assistant Professor of Urban Planning and Development
Institution: Addis Ababa University College of Natural and Computational Science
Course Level: Freshman Course
Date: January 2021
Learners will be able to:
Describe major drainage systems in Ethiopia and the Horn.
Examine surface and ground water resource potentials.
Recognize economic potentials of the water sector in Ethiopia.
Earth's Surface: 71% covered by water, mostly seas and oceans.
Water Composition:
97.5% saline (oceans and seas)
2.5% fresh water
68.7% in glaciers
30.1% in ground water
0.8% in permafrost
0.4% in surface water
Types: Lakes, rivers, atmosphere, soils, wetlands are surface waters.
Distribution Issues:
Unevenly distributed due to:
Latitudinal variations
Climatic conditions
Topographic setups
Ethiopia's Water Resources: Large volume of ground and surface water due to diverse topography and higher rainfall; recognized as the "water tower of Eastern Africa."
Concept of Drainage: Water flows through well-defined channels.
Components: Principal river and tributaries.
Regions: Separated by water divides, resulting from geological processes and topography.
Western Drainage System
Southeastern Drainage System
Rift Valley Drainage System
Significance: Largest drainage system, drains 40% of Ethiopia, carrying 60% of annual water flow.
Major River Basins:
Tekeze River
Abay River
Baro-Akobo River
Ghibe (Omo) River
Characteristics:
Largest river by discharge and area (199,812 km²).
Flows approximately 1,450 km from Lake Tana to join White Nile.
Streams: More than 60 streams drain Abay, including Ghilgel Abay (Little Abay).
Details:
Drains 82,350 km².
Significant erosion resulting in varied topography.
Flows into Sudan as Atbara River.
Baro-Akobo: Drains wettest highlands, covers 75,912 km².
Ghibe/Omo: Drains 79,000 km²; both contribute to Sobat River in South Sudan.
Major Rivers: Wabishebelle and Ghenale, originating from Arsi, Bale, Sidama, and Harerghe plateaus.
Ghenale River Basin: 171,042 km², named Juba in Somalia.
Wabishebelle River Basin: 202,697 km², does not reach Indian Ocean.
Characteristics: Low rainfall, high evaporation.
Major River: Awash River with 114,123 km² basin area.
Flow Direction: Streams flow in multiple directions, ending in interconnected lakes/marshes.
Afar Drainage: Very low stream flow, characterized by high evaporation.
Southern Rift Valley: Features lakes with streams supplying water.
Ethiopia has many rivers originating in highlands, forming major watersheds.
Typically originate above 1500 meters a.s.l.
Transboundary nature.
Seasonal fluctuations due to rainfall patterns.
Types: Highland lakes, rift valley lakes, and man-made lakes.
Significant Lakes: Lake Tana, crater lakes, and dams.
Lower groundwater potential, estimated between 12-30 BMC.
High potential for hydroelectric generation, estimated at 45,000 MW.
Significant Projects:
GERD: Aims for 6,400 MW.
Gilgel Gibe III: Operational with 1,870 MW.
Rugged terrain limits river use for irrigation and transport; Baro is only navigable river.
Rich fisheries, main production from Lake Tana & Lake Chamo.
Lakes provide recreational opportunities and necessary resources.
Discuss the major drainage systems of Ethiopia.
Explain the hydroelectric and fishing potential of Ethiopian water resources.
State the major characteristics of Ethiopian rivers.