Dataset Restricted Access

Hydro and sediment dyanamics on a laboratory scaled fringing reef: morphology simulations

Pomeroy, Andrew William MacKay


DataCite XML Export

<?xml version='1.0' encoding='utf-8'?>
<resource xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.1/metadata.xsd">
  <identifier identifierType="DOI">10.5281/zenodo.236754</identifier>
  <creators>
    <creator>
      <creatorName>Pomeroy, Andrew William MacKay</creatorName>
      <givenName>Andrew William MacKay</givenName>
      <familyName>Pomeroy</familyName>
      <affiliation>The University of Western Australia</affiliation>
    </creator>
  </creators>
  <titles>
    <title>Hydro and sediment dyanamics on a laboratory scaled fringing reef: morphology simulations</title>
  </titles>
  <publisher>Zenodo</publisher>
  <publicationYear>2015</publicationYear>
  <subjects>
    <subject>Fringing reef</subject>
    <subject>Coral reef</subject>
    <subject>Sediment transport</subject>
    <subject>Waves</subject>
    <subject>Suspended sediment concentration</subject>
  </subjects>
  <dates>
    <date dateType="Issued">2015-02-17</date>
  </dates>
  <resourceType resourceTypeGeneral="Dataset"/>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://zenodo.org/record/236754</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="References">10.1016/j.coastaleng.2015.01.005</relatedIdentifier>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsVersionOf">10.5281/zenodo.724360</relatedIdentifier>
  </relatedIdentifiers>
  <rightsList>
    <rights rightsURI="info:eu-repo/semantics/restrictedAccess">Restricted Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">&lt;p&gt;A laboratory experiment was conducted to investigate the dynamics of cross-shore sediment transport across a&lt;br&gt;
fringing coral reef. The aim was to quantify how a highly bimodal spectrum of high-frequency (sea-swell) and&lt;br&gt;
low-frequency (infragravity and seiching) waves that is typically present on coral reef flats, influences the&lt;br&gt;
various sediment transport mechanisms. The experiments were conducted in a 55 m wave flume, using a 1:15&lt;br&gt;
scale fringing reefmodel that had a 1:5 forereef slope, a 14 m long reef flat, and a 1:12 sloping beach. The initial&lt;br&gt;
7 m of reef flat had a fixed bed, whereas the back 7 m of the reef and the beach had a moveable sandy bed. Four&lt;br&gt;
seven-hour irregular wave cases were conducted both with and without bottom roughness elements (schematically&lt;br&gt;
representing bottom friction by coral roughness), as well as for both low and high still water levels.&lt;/p&gt;

&lt;p&gt;More information about this experiment is available in the methods of the associated publication (http://doi.org/10.1016/j.coastaleng.2015.01.005).&lt;/p&gt;</description>
    <description descriptionType="Other">Instrument metadata is contained within each NetCDF file. 
Please contact the authors if any further clarification is required.</description>
  </descriptions>
</resource>
26
0
views
downloads
All versions This version
Views 2626
Downloads 00
Data volume 0 Bytes0 Bytes
Unique views 2121
Unique downloads 00

Share

Cite as