<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>J. H. List</dc:contributor>
  <dc:contributor>G. Gelfenbaum</dc:contributor>
  <dc:contributor>R. P. Stumpf</dc:contributor>
  <dc:contributor>M. Hansen</dc:contributor>
  <dc:creator>A. H. Sallenger Jr.</dc:creator>
  <dc:date>1995</dc:date>
  <dc:description>On a clear calm evening during July 1992, an anomalously large wave, reportedly 6 m high struck the Daytona Beach, Florida area. It is hypothesized that a squall line and associated pressure jump, travelling at the speed of a free gravity wave, coupled resonantly with the sea surface forming the large wave or "squall-line surge'. The wave was forced along the length of the squall line, with the greatest amplitude occurring at the water depth satisfying the resonant condition. -from Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:title>Large wave at Daytona Beach, Florida, explained as a squall-line surge</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>