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Part of the book series: Water Science and Technology Library ((WSTL,volume 16))

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Abstract

The prediction of extreme floods associated with different recurrence intervals has always been a difficult task. Even the alternative of estimating maximum probable floods is fraught with uncertainty. The methodology is not yet standardized and the datums and factors to consider are not all incorporated in any single procedure for estimating these floods. The estimates are even more difficult in areas with limited data. Developing areas in particular have sparse hydrological networks and the spectrums of floods gauged in these areas provide limited, if not at times misleading, information. Rain data are often more reliable and more extensive and therefore many methods for estimating floods use rainfall data. The paper compares alternative methods such as the rational method, unit hydrograph method, soil conservation method, and empirical methods. Owing to wide variations in topography and climate over large catchments it is demonstrated that many of these methods cannot be scaled up or extrapolated. It appears catchment modelling using hydraulic techniques is the most reliable where extrapolation is required. Various empirical methods of estimating extreme floods are compared and it is shown that for large catchments available data illustrates the floods converge to common figures whichever data are used.

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References

  • Balek, J. 1977. Hydrology and Water Resources in Tropical Africa. Elsevier.

    Google Scholar 

  • Bhalotra, Y.P.R. 1987. Climate of Botswana. Part II Elements of Climate: 1: Rainfall. Dept.Met. Services, Botswana.

    Google Scholar 

  • Creager, W.P., Justin, J.D. and Hinds, J., 1964. Engineering for dams. Wiley.

    Google Scholar 

  • Francou, J. and Rodier, J.A. 1967. ‘.Essai de classification des crues maximales’. Proc.Leningrad Symp. on floods and their computation. UNESCO.

    Google Scholar 

  • Hydrological Research Unit, 1972. Design Flood Determinations in South Africa. University of the Witwatersrand.

    Google Scholar 

  • Institute of Hydrology, 1986. A review of flood estimates for Kolobeng and Metsemotlhaba dams. For Alexander Gibb and Partners, Botswana. Wallingford.

    Google Scholar 

  • Kovacs, G. 1971. Relationship between characteristic flood discharges and catchment area.Symp. Role of hydrology in developing Africa II. WMO No. 301, pp 18–23.

    Google Scholar 

  • Kovacs, Z.P. 1988. Regional maximum Flood Peaks in Southern Africa. TR137, Dept. Water Affairs, Pretoria.

    Google Scholar 

  • Mitchell, T.B. Nov 1974. ‘A study of Rhodesian floods and proposed flood formulae’. The Rhodesian Engineer.

    Google Scholar 

  • Op Ten Noort, T. and Stephenson, D. 1982. Flood peak calculation in South Africa. Water Systems Research Group, University of the Witwatersrand.

    Google Scholar 

  • Pegram, G. and Adamson, P. 1988. ‘Revised risk analysis for extreme storms and floods in Natal’. Civil Engineer in S.A.. Jan. pp 15–42. Discussion July, pp 331–6.

    Google Scholar 

  • Pitman, W.V. and Midgley D.C. Aug. 1967. “Flood studies in South Africa : Frequency analysis of peak discharges”. The Civil Engineer in S.A.

    Google Scholar 

  • Rodier, J.A. and Roche, M. 1988. World catalogue of maximum observed floods. IAHS public 143.

    Google Scholar 

  • Smith, A.M. 1991. ‘Extreme Palaeofloods, their climatic significance and the chances of similar floods re-occurring’. SA. Journal of Science. 87 (6) 219–220.

    Google Scholar 

  • Stephenson, D. July 1983. ‘Hydrological Myths’. The Civil Engineer in SA. 337–383.

    Google Scholar 

  • Stephenson, D. and Meadows,M.E. 1986. Kinematic Hydrology and Modelling. Elsevier.

    Google Scholar 

  • Stephenson, D. and Collins, S.T. 1988. ‘Problems due to inaccurate flood estimates at Collywobbles’. Proc. Intl. Congress on Large dams. San Francisco.

    Google Scholar 

  • Van der Leeden, F. 1975. Water Resources of the World. Water Information Cr. NY.

    Google Scholar 

  • World Meterological Organization (WMO) 1983. Guide to Hydrological Practices. Vol. II.Analysis. Forecasting and other Applications. 4th Edn. Geneva, WMO 168.

    Google Scholar 

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© 1996 Springer Science+Business Media Dordrecht

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Stephenson, D. (1996). Estimation of Extreme Floods with Particular Reference to Southern Africa. In: Singh, V.P., Kumar, B. (eds) Proceedings of the International Conference on Hydrology and Water Resources, New Delhi, India, December 1993. Water Science and Technology Library, vol 16. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-0389-3_33

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  • DOI: https://doi.org/10.1007/978-94-011-0389-3_33

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-4174-4

  • Online ISBN: 978-94-011-0389-3

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