<?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:date>1945</dc:date>
  <dc:description>&lt;p&gt;In May 1943, Illinois was subjected to a series of flood that reached&amp;nbsp;major intensities in the central part of the state but decreased to&amp;nbsp;minor intensity--less than the maximum for the year--in the northwestern and extreme southern part. All records were broken on lower&amp;nbsp;Illinois River and on its triibutaries entering from the east, from Sangamon River south, as well as on Kaskaskia River. These floods&amp;nbsp;were the result of rain during the storm period May 6-21. At no&amp;nbsp;place did it rain continuously for 24 hours and in most places the limit&amp;nbsp;was about half a day. An appropriate description is a series of showers&amp;nbsp;that produced a series of floods on small streams. As the rains&amp;nbsp;continued, the ground became more nearly saturated and the ratio of&amp;nbsp;runoff to rainfall increased. As the small streams entered larger ones,&amp;nbsp;with their peaks arriving at different times, the channel storage of&amp;nbsp;the larger streams smoothed out the minor peaks so that the very large streams had only one peak. The magnitude of channel storage in&amp;nbsp;Illinois River and its adjoining lakes is emphasized by the fact that&amp;nbsp;the peak discharge at Meredosia, lasting&amp;nbsp;about 44 hours, was no greater&amp;nbsp;than the peak discharge of Sangamon River at Oakford, 123,000 second-feet, that lasted about an hour.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Illinois Division of Waterways</dc:publisher>
  <dc:title>The floods of May 1943 in Illinois</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>