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Impact Assessment of Mtera and Kidatu Reservoirs on the Annual Maximum Floods at Stiegler's Gorge of the Rufiji River in Tanzania
The impoundment of any river causes changes in the downstream flow regime. The effect of a dam on flow regime depends on both the storage capacity of the reservoir relative to the volume of river flow and the way the dam is operated. The most common attribute of flow regulation is a decrease in the...
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Published in: | Water international 2006-03, Vol.31 (1), p.100-108 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The impoundment of any river causes changes in the downstream flow regime. The effect of a dam on flow regime depends on both the storage capacity of the reservoir relative to the volume of river flow and the way the dam is operated. The most common attribute of flow regulation is a decrease in the magnitude of the flood peaks and an increase in low flows. This paper reports the findings of a study to assess the cumulative impact of two dams on the Great Ruaha River in Tanzania (the Mtera and Kidatu Reservoir System) on flood flows. The method used was to compare the observed annual maximum flows at downstream locations after the construction of the dams with mathematically modeled estimates of the annual maximum flows at the same locations, assuming that the dams were not built (i.e. generating naturalized flows). Contrary to expectations, the study found that annual maximum peaks were supposed to be less than those actually observed. For instance, in 1989, annual maximum peak flow of 1,400 m
3
/s was recorded at Kidatu, but the estimated uncontrolled peak flow should have been 800 m
3
/s, signifying an artificially-induced flood wave. Although, there was a significant impact on the peak flows at Kidatu awing to the dams, the impact was found to be minimal on the flow peaks at Steigler's Gorge. |
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ISSN: | 0250-8060 1941-1707 |
DOI: | 10.1080/02508060608691919 |