<?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>T. Ohtake</dc:contributor>
  <dc:creator>A. G. Fountain</dc:creator>
  <dc:date>1985</dc:date>
  <dc:description>The results indicate a seasonal variation in nucleus concentration with a winter minimum and a north-to-south trend in the increasing average concentration. Some episodes of high concentrations were correlated with 500 mb isobaric transport from Eurasia and 700 mb cyclogenesis over Alaska. These results suggest that local nucleus sources play a dominant role in the seasonal variation, while some individual episodes are caused by external or regional influences. -from Authors</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1175/1520-0450(1985)024&lt;0377:CASAOI&gt;2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Concentrations and source areas of ice nuclei in the Alaskan atmosphere.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>