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  <titleInfo>
    <nonSort>The </nonSort>
    <title>applicability of tank model to monthly rainfall-runoff relationship</title>
  </titleInfo>
  <name type="personal">
    <namePart>Uddin, A. B. M. Kamal</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Arbhabhirama Anat</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Selvalingam, Selvadore</namePart>
    <role>
      <roleTerm type="text">Co-Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart> Tawatchai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Australia Government</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>1977</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">print</form>
    <extent>73 p.</extent>
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  <abstract>A structure of the Tank Model as conceived by Prof. Sugawara was fixed. Continuous records of monthly rainfall and mean monthly or monthly evaporation, as well as physical parameters were the inputs to the model. The model parameters were initially given from previous experience and later adjusted so that the computed hydrographs reasonably agree with the observed hydrographs. The model was then used to predict  hydrographs to compare the results with the observed ones.  The obtained results were fairly reasonable for the Nan river  basin at Sirikit Dam and the Yorn river basin at Kaeng Luang but were not so good for t he Khwae Noi river basin at Lum Sum. This may be due to large areal fluctuation of precipitation and small number of rainfall  stations in the basin. Although individual year peak and volume of runoff could not be predicted accurately, total volume of discharge for several years could be predicted with fair accuracy.</abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering of the Asian Institute of Technology, Bangkok, Thailand</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1978</note>
  <subject authority="lcsh">
    <topic>Runoff</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Hydrologic models</topic>
  </subject>
  <relatedItem type="series">
    <titleInfo>
      <title>Thesis ; no. 929</title>
    </titleInfo>
    <name type="corporate">
      <namePart>Asian Institute of Technology.</namePart>
      <namePart/>
    </name>
  </relatedItem>
  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B22645</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B22645</url>
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    <recordCreationDate encoding="marc">200198</recordCreationDate>
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