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  <titleInfo>
    <title>Applicability of some statistical distributions in hydrology</title>
  </titleInfo>
  <name type="personal">
    <namePart>Jivajirajah, Thambirajah</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Huynh Ngoc Phien</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Hoshi, Kiyoshi</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Suphat 'Vongvisessomjai</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Royal Government of Netherlands</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1982</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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    <extent>v, 73 p.</extent>
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  <abstract>Three statistical distributions namely log Pearson type- 3, Johnson's Sb and transformed gamma distributions-were considered in order to investigate their applicability to hydrology with regards to their flexibility and difficulties in estimating the parameters. Log Pearson type-3 distribution  was applied t o annual streamflow, annual rainfall , annual flood peaks and  annual maximum rainfall its parameters were estimated using seven different  methods. Johnson' s Sb and transformed gamma distributions were applied to  annual streamflow and Annual rainfall, since these are bounded on both sides. Two and four methods for parameters estimation were employed to  transformed gamma and SB distributions respectively. It was found that the log Pearson type- 3 distribution using method of  mixed moments for its parameter estimation is superior for the application in hydrology. However, care should be taken in using the log Pearson type-3  distribution in flood analysis, as it in most of the cases tends to have an upper bound. The transformed gamma distribution was found to be better than the Sb distribution in both annual streamflow and annual rainfall . </abstract>
  <note>A thesis submitted in partial fulfillment of the requirement for the degree of Master of Engineering, school of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1982</note>
  <subject authority="lcsh">
    <topic>Hydrology</topic>
    <topic>Statistical methods</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WA-83-4</title>
    </titleInfo>
    <name type="corporate">
      <namePart>Asian Institute of Technology.</namePart>
      <namePart/>
    </name>
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  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B21405</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B21405</url>
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