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  <titleInfo>
    <title>Annual water balance in a snow region</title>
  </titleInfo>
  <name type="personal">
    <namePart>Zhang, Zitai</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
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  </name>
  <name type="personal">
    <namePart>Kazama, So</namePart>
    <role>
      <roleTerm type="text">Chairperson    </roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Tswatchai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Examination committee           </roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Kubo, Naritaka</namePart>
    <role>
      <roleTerm type="text">Examination committee           </roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Education Committee. The People's Republic of China</namePart>
    <role>
      <roleTerm type="text">Scholarship donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <genre authority="marc">theses</genre>
  <originInfo>
    <place>
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    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1998</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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  <physicalDescription>
    <extent>57 leaves</extent>
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  <abstract>The Taki dam river basin is a very heavy snowfall region with many observing stations  in the center part of Japan. In order to analyze water balance of a region with snowfall which  results runoff delay due to snow storage and snow melt, the Taki dam river basin was selected  for the study purpose.  The water balance deals with the analysis which balances the continuity equation for a  basin on an average basis and on dynamic basis. Using daily rainfall , daily temperature ,  runoff and snowdepth with elevation over the basin as input data, a water balance was derived  for upper Taki dam river basin. Evapotranspiration , most important element was computed by  Thomethwaite method and Hamon method and the suitability of the empirical equations in the  snow region was examined. The regression equations were obtained from the observation data  relating snowfall, snow depth and elevation for the precipitation correction. The results are for  surface compared with actual runoff in order to determine the water balance in the Taki dam  river basin from 1988 to 1994.</abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering, School of Civil Engineering</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1998</note>
  <subject authority="lcsh">
    <topic>Water balance (Hydrology)</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WM-97-09</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=B13290</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B13290</url>
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