Characterisation of the Flow Regime of Ewaso Ngiro North River

This study aimed at characterising the river flow regime using statistical and probability methods. Streamflow data for Archers Post river gauging station for the period 1960 to 1998 were used for the analysis. Preliminary analysis of the daily flow data was undertaken to determine monthly mean flow...

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Published inEast African agricultural and forestry journal Vol. 65; no. 1-2; pp. 71 - 78
Main Authors Gichuki, FN, Gichuki, PG, Muni, RK
Format Journal Article
LanguageEnglish
Published Taylor & Francis 01.07.1999
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Abstract This study aimed at characterising the river flow regime using statistical and probability methods. Streamflow data for Archers Post river gauging station for the period 1960 to 1998 were used for the analysis. Preliminary analysis of the daily flow data was undertaken to determine monthly mean flow, annual mean flow, 7, 30, 90 and 120 days mean low flow and highest daily discharge (flood flow) for each year. Descriptive statistical parameters including: the mean, standard error, median, standard deviation, coefficient of variation, kurtosis, skewness and confidence level of mean at 95% were computed. The cumulative distribution function of the monthly flow showed that February had the lowest flow and November had the highest. Monthly flow analysis revealed that there were three peaks in April, August and November corresponding to the long, continental and short rainy seasons.
AbstractList This study aimed at characterising the river flow regime using statistical and probability methods. Streamflow data for Archers Post river gauging station for the period 1960 to 1998 were used for the analysis. Preliminary analysis of the daily flow data was undertaken to determine monthly mean flow, annual mean flow, 7, 30, 90 and 120 days mean low flow and highest daily discharge (flood flow) for each year. Descriptive statistical parameters including: the mean, standard error, median, standard deviation, coefficient of variation, kurtosis, skewness and confidence level of mean at 95% were computed. The cumulative distribution function of the monthly flow showed that February had the lowest flow and November had the highest. Monthly flow analysis revealed that there were three peaks in April, August and November corresponding to the long, continental and short rainy seasons.
Author Muni, RK
Gichuki, FN
Gichuki, PG
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Copyright 1999 Taylor and Francis Group, LLC 1999
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References Akonga J Downing TE (CIT0001) 1987
Gupta B. (CIT0004) 1991
Gichuki FN Liniger (CIT0003) 1998; 8
Viessman W Lewis LG (CIT0007) 1989
Chow VT (CIT0002) 1988
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  year: 1998
  ident: CIT0003
  publication-title: Eastern and Southern Africa Geographical Journal
  contributor:
    fullname: Gichuki FN Liniger
– volume-title: Engineering Hydrology.
  year: 1991
  ident: CIT0004
  contributor:
    fullname: Gupta B.
– volume-title: Applied Hydrology
  year: 1988
  ident: CIT0002
  contributor:
    fullname: Chow VT
– volume-title: The effects of climatic variations on agriculture in central and eastern Kenya.
  year: 1987
  ident: CIT0001
  contributor:
    fullname: Akonga J Downing TE
– volume-title: Introduction to Hydrology
  year: 1989
  ident: CIT0007
  contributor:
    fullname: Viessman W Lewis LG
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StartPage 71
Title Characterisation of the Flow Regime of Ewaso Ngiro North River
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