<?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>G.E. Koberg</dc:creator>
  <dc:description>&lt;p&gt;&lt;span&gt;By means of the energy-budget method, measurements of&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;evaporation&lt;/span&gt;&lt;span&gt;&amp;nbsp;losses from four&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;reservoirs&lt;/span&gt;&lt;span&gt;&amp;nbsp;on&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Salt&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;River&lt;/span&gt;&lt;span&gt;, Ariz., were determined to range from 57.5 to 69.9 inches for the 12-month period April 1958 to March 1959. Water is withdrawn from Roosevelt Lake at considerable depth and released through three run-of-the-&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;river&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;reservoirs&lt;/span&gt;&lt;span&gt;. Because the water released from Roosevelt Lake is cold,&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;evaporation&lt;/span&gt;&lt;span&gt;&amp;nbsp;losses from the downstream&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;reservoirs&lt;/span&gt;&lt;span&gt;&amp;nbsp;are considerably lower than those from Roosevelt Lake.&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Evaporation&lt;/span&gt;&lt;span&gt;&amp;nbsp;pan coefficients computed for the various&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;reservoirs&lt;/span&gt;&lt;span&gt;&amp;nbsp;ranged from 0.53 to 0.65. A base&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;evaporation&lt;/span&gt;&lt;span&gt;&amp;nbsp;rate was computed for each&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;reservoir&lt;/span&gt;&lt;span&gt;&amp;nbsp;as the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;evaporation&lt;/span&gt;&lt;span&gt;&amp;nbsp;rate that would have occurred had there been no change in energy storage and the net advected energy equalled zero during the year.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1080/02626666009493178</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Taylor &amp; Francis</dc:publisher>
  <dc:title>Effect on evaporation of releases from reservoirs on Salt River, Arizona</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>