<?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:creator>E.J. Pluhowski</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;High-altitude photography provides an effective method of&amp;nbsp;monitoring the spatial extent of turbidity plumes in Lake Ontario.&amp;nbsp;Large plumes generated by the Niagara, Genesee, and Oswego Rivers are&amp;nbsp;identifiable on photographs obtained from about 60,000 feet above the&amp;nbsp;lake on July 6, 1970, October 19, 1970, and May 29, 1971. The&amp;nbsp;Niagara plume, covering as much as 43 sq mi of the lake's surface, is the&amp;nbsp;largest turbidity feature. The configuration of the plumes is a function&amp;nbsp;of river discharge, level of turbidity, and wind speed and direction.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Remote sensing of turbidity plumes in Lake Ontario</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>