<?xml version="1.0" encoding="UTF-8"?>
<mods xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://www.loc.gov/mods/v3" version="3.1" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-1.xsd">
  <titleInfo>
    <title>Tidal current at Songkla lagoon inlet</title>
  </titleInfo>
  <name type="personal">
    <namePart>Kathirgamanathan, Murugesu</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>Tawatchai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Co-Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Nishimura, Hitoshi</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>The Government of United Kingdom</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>1976</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">print</form>
    <extent>64 p.</extent>
  </physicalDescription>
  <abstract>A tidal mathematical model was developed for the Songkla lagoon inlet, Thailand. Due to the tidal fluctuations, the flow in the inlet channel was unsteady. The node and branch method of computation was used in  constructing the model. The governing equations of the unsteady flow were linearized and a computer program was developed to solve the linearized  equations. The model was calibrated using the short measurement period of data available. The boundary conditions required for the model were the water stages at both end of the channel. The current velocities were predicted for a 4 months period using the data of the boundary conditions and calibrated Mannings' coefficient.  Harmonic analysis was done for water stage and current velocity  data using the parameters obtained from the analysis, the current velocity was predicted using the data of water level fluctuation. The results from  the both methods are compared with measured values. Al though the node and branch method was originally used in channel networks, it is found to be applicable to the tidal flow calculations, in which the flow is actually not unidirectional. This method gives reasonably good results when the data of the boundary conditions are accurate.</abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering at the Asian Institute of Technology, Bangkok, Thailand. </note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1976</note>
  <subject authority="lcsh">
    <topic>Ocean currents</topic>
    <topic>Songkla lagoon</topic>
  </subject>
  <relatedItem type="series">
    <titleInfo>
      <title>Thesis ; no. 858</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=B23675</identifier>
  <location>
    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B23675</url>
  </location>
  <recordInfo>
    <recordCreationDate encoding="marc">140198</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260819084615.0</recordChangeDate>
  </recordInfo>
</mods>
