Journal of Spatial Hydrology Volume 7 Number 1 Article 4 2007 Hydrodynamics of topographically closed lakes in the Ethio- Kenyan Rift: The case of lakes Awassa and Naivasha Follow this and additional works at: https://scholarsarchive.byu.edu/josh BYU ScholarsArchive Citation (2007) "Hydrodynamics of topographically closed lakes in the Ethio-Kenyan Rift: The case of lakes Awassa and Naivasha," Journal of Spatial Hydrology: Vol. 7 : No. 1 , Article 4. Available at: https://scholarsarchive.byu.edu/josh/vol7/iss1/4 This Article is brought to you for free and open access by the Journals at BYU ScholarsArchive. It has been accepted for inclusion in Journal of Spatial Hydrology by an authorized editor of BYU ScholarsArchive. For more information, please contact
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[email protected]. Journal of Spatial Hydrology Vol.7, No.1, Spring 2007 Hydrodynamics of topographically closed lakes in the Ethio-Kenyan Rift: The case of lakes Awassa and Naivasha Tenalem Ayenew1*, Robert Becht2, Arno van Lieshout2, Yemane Gebreegziabher3, Dagnachew Legesse1, Japheth Onyando4 Abstract The hydrodynamics and the long-term water balance of two topographically closed crater lakes is presented in a comparative manner using a spread-sheet hydrological model. The main objective of the work is to study the role of groundwater and the effect of water abstraction from lakes Awassa and Naivasha. The rationale of selection of the two lakes separated by thousands of kilometers is the striking similarity of their hydrogeological and geomorphological setting and future intended water uses for large-scale abstraction from the lakes and feeder rivers. The net groundwater outflow from Lake Awassa and the effect of water abstraction from Lake Naivasha under different scenarios were calculated based upon the average monthly hydrometeorological data of rainfall, evaporation and river inflows.