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  <titleInfo>
    <title>Analysis of return periods maximum flood levels of Chao Phraya River in Bangkok</title>
  </titleInfo>
  <name type="personal">
    <namePart>Jirawat Ganasut</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
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  </name>
  <name type="personal">
    <namePart>Tawatchai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
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  <name type="personal">
    <namePart>Huynh, Ngoc Phien</namePart>
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      <roleTerm type="text">Examination Committee</roleTerm>
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  <name type="personal">
    <namePart>Nielsen, Steen Asger</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Government of Australia</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
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    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1988</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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    <extent>117 p.</extent>
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  <abstract>Flocy model . The model is  developed to calculate the flood frequency at any station along  the study reach from Bangsai to the river mouth at Fort Chula  using theod frequencies in the Chao Phraya River have been studied  by means of a coincident flood frequen total probability theorem. The frequency and duration  relations of the upstream and downstream water levels are used as  the boundary conditions. The Single Reach with Loop Model is  applied to calculate a relationship of maximum flood level at any  station as a function of the Bangsai flood peak level and the  tides at Fort Chula. The calibration is made by adjusting the  duration curve to allow it to represent very large flood events.  Good agreement between the computed flood-stage frequency curves  and the observed one are obtained.  After calibration, the model is applied to determine the  effects of a flood control diversion channel which diverts flood  discharge at Pak Kret on the we s t bank of the Chao Phraya River.  This measure is found to reduce the flood level frequency in the  upper reach efficiently. For the lower reach , it is found not  capable enough to reduce the flood level frequency effectively . </abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering, School of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1988</note>
  <subject authority="lcsh">
    <topic>Floods</topic>
    <topic>Thailand</topic>
    <topic>Chao Phraya River</topic>
    <topic>Mathematical models</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WA-88-5</title>
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      <namePart>Asian Institute of Technology.</namePart>
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    </name>
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  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B18853</identifier>
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