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  <titleInfo>
    <title>Equilibrium bay shape approach for analysis of shoreline in Myanmar</title>
  </titleInfo>
  <name type="personal">
    <namePart>Khin Nathar Aung Myint Htay</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Sutat Weesakul</namePart>
    <role>
      <roleTerm type="text">Chairperson </roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Babel, Mukand Singh</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Sarawut Ninsawat</namePart>
    <role>
      <roleTerm type="text">Examination committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Somchai Chonwattana</namePart>
    <role>
      <roleTerm type="text">Examination committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>DAAD</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <genre authority="marc">series</genre>
  <genre authority="marc">technical report</genre>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Pathum Thani, Thailand</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>2019</dateIssued>
    <issuance>continuing</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <extent>79 leaves : ill. (some col.) + 1 online resource</extent>
  </physicalDescription>
  <abstract>Total of 106 bays along the coastline of Myanmar are analyzed using equilibrium bay shape  equation in this study and are classified into three groups: static equilibrium (SEB), dynamic  equilibrium (DEB) and unstable. Only the geometrical planform which can be obtained from  satellite images is used for the analysis of this study.  Littoral cells along the coastline of Myanmar are identified based on the geographical planform  only. Analysis of equilibrium bays in the littoral cells is conducted in order to identify the areas  where erosion or accretion can occur as well as long term equilibrium can exist. Areas where  changes in the sediment supply can affect the stability of the shoreline planform are also  determined. Some characteristics of the bays are compared and contrast to those of bays in  neighbouring countries (Thailand and Vietnam) using the results of previous studies in order to  indicate the overall shoreline changes along the continuous shoreline.  For the stabilization of the unstable bays, two methods are proposed: headland control method and  sediment control method. Headland control method is to adjust the upcoast control point and it can  be used for both static and dynamic condition. Both methods are used for the stabilization of  dynamic unstable bays and the efficiency index (El) of using each method is compared. </abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering in Water Engineering and Management</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 2019</note>
  <subject authority="lcsh">
    <topic>Equilibrium (Physiology)</topic>
    <topic>Analysis</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Equilibrium</topic>
    <geographic>Myanmar</geographic>
  </subject>
  <subject authority="lcsh">
    <topic>Shorelines</topic>
    <geographic>Myanmar</geographic>
  </subject>
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    <titleInfo>
      <title>Thesis;  no. WM-19-13</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=B06419</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B06419</url>
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    <recordCreationDate encoding="marc">200903</recordCreationDate>
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