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  <skos:Concept rdf:about="c82f3480-545f-4491-83f1-0477369ddcd8">
    <skos:broader rdf:resource="376a1d5c-2496-4381-981f-bc047af92044"/>
    <skos:prefLabel xml:lang="en">PERMAFROST</skos:prefLabel>
    <skos:changeNote>Date=2015-12-10 User Id=aaleman Entity=NarrowerRelation Operation=INSERT 
User Note=Insert Concept
System Note=add narrower relation
New Value=PERMAFROST [c82f3480-545f-4491-83f1-0477369ddcd8,84051] - PERMAFROST TEMPERATURE [d8606e80-3d34-4540-a355-5f99737f7ab7,158553]</skos:changeNote>
    <gcmd:reference gcmd:text="American Meteorological Society Glossary of Meteorology Online: &apos;http://amsglossary.allenpress.com/glossary&apos;" xml:lang="en"/>
    <skos:narrower rdf:resource="d8606e80-3d34-4540-a355-5f99737f7ab7"/>
    <skos:definition xml:lang="en">1. (Also called perennially frozen ground, pergelisol, permanently frozen
ground.) A layer of soil or bedrock at a variable depth beneath the surface of
the earth in which the temperature has been below freezing continuously from a
few to several thousands of years. Permafrost exists where the summer heating
fails to descend to the base of the layer of frozen ground. A continuous
stratum of permafrost is found where the
annual mean temperature is below about 5C (23F). &lt;p&gt;2. As limited in
application by P. F. Svetsov, soil that is known to have been frozen for at
least a century. &lt;p&gt;
Muller, S. W., 1947: Permafrost, or Permanently Frozen Ground, and
Related Engineering Problems, &lt;p&gt;
Hare, F. K., 1951: Compendium of Meteorology, p. 958, and map, p.
956.</skos:definition>
    <dcterms:modified>2015-12-10 17:11:34.0</dcterms:modified>
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