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  <titleInfo>
    <title>Wind driven current profile in the presence of different boundaries</title>
  </titleInfo>
  <name type="personal">
    <namePart>Chen, Ching-yu</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Suphat Vongvisessomjai</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Prida Thimakorn</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Gupta, Ashim Das</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Ret-Ser Engineering Agency (R.O.C.)</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>1979</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">print</form>
    <extent>viii, 63 p.</extent>
  </physicalDescription>
  <abstract>The wind induced flow phenomena especially the surface drift currents in a closed basin are investigated. The laboratory experiments of such  phenomena have been made under various wind velocities and different boundary conditions. The measurements include the wind profiles over the water surface, the drift current profile, the characteristics of waves. The general shape of drift current profiles was changed with various wind velo city and different boundary conditions. The point of zero drift currents on an average is 20 percent of the total depth bel ow water surface in spite  of various wind velocities under different boundary conditions. The logarithmic distribution of drift current profile holds for both downwind and reversed direction but not continuously. The mean water surface set-up variation is a main role controlling return flow. The research will be useful for the understanding of movement of oil slicks and transports of pollutants. </abstract>
  <note>A thesis submitted in partial fulfillment of requirements for the degree of master of engineering, School of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1980</note>
  <subject authority="lcsh">
    <topic>Ocean currents</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WA-79-31</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=B22183</identifier>
  <location>
    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B22183</url>
  </location>
  <recordInfo>
    <recordCreationDate encoding="marc">130598</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260819090806.0</recordChangeDate>
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