<?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>David J. Parsons</dc:contributor>
  <dc:creator>Thomas J. Stohlgren</dc:creator>
  <dc:date>1987</dc:date>
  <dc:description>Sequoia National Park has monitored wet deposition chemistry in conjunction with the National Atmospheric Deposition Program and National Trends Network (NADP/NTN), on a weekly basis since July, 1980. Annual deposition of H, NO&lt;sub&gt;3&lt;/sub&gt; and SO&lt;sub&gt;4&lt;/sub&gt; (0.045, 3.6, and 3.9 kg ha&lt;sup&gt;−1&lt;/sup&gt; a&lt;sup&gt;−1&lt;/sup&gt;, respectively) is relatively low compared to that measured in the eastern United States, or in the urban Los Angeles and San Francisco areas. Weekly ion concentrations are highly variable. Maximum concentrations of 324,162, and 156 μeq &lt;i&gt;ol&lt;/i&gt;&lt;sup&gt;−1&lt;/sup&gt; of H, NO&lt;sub&gt;3&lt;/sub&gt; and SO&lt;sub&gt;4&lt;/sub&gt; have been recorded for one low volume summer storm (1.4 mm). Summer concentrations of NO&lt;sub&gt;3&lt;/sub&gt; and SO&lt;sub&gt;4&lt;/sub&gt; average two and five times higher, respectively, than concentrations reported for remote areas in the world. There is considerable variability in the ionic concentration of low volume samples, and much less variability in moderate and high volume samples.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/0004-6981(67)90084-4</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Pergamon Press</dc:publisher>
  <dc:title>Variation of wet deposition chemistry in Sequoia National Park, California</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>