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  <dc:title xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Copenheaver - Stadium Woods - QUAL - ITRDB VA037</dc:title>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Copenheaver, C.A.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Copenheaver, C.A.</dc:creator>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">QUAL</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Quercus alba L.</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">white oak</dc:subject>
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  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/tree ring (total ring width,null,null,millimeter,null,tree ring,null,null,N,Tree ID: 350; units are 0.01 mm if end-of-series marker is 999 and 0.001 mm if end-of-series marker is -9999)</dc:subject>
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  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows"> (Stadium Woods&gt;LATITUDE 37.222886&gt;LONGITUDE -80.219421)</dc:subject>
  <dc:description xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">On the Virginia Tech campus, adjacent to the football stadium is a 4.6-ha forest fragment that contains a population of unusually large white oak (Quercus alba L.) trees. We used dendroecology and sampled vegetation in fixed area plots to reconstruct the disturbance history of this forest fragment and compared the radial-growth averaging criteria and the boundary-line release criteria for identifying canopy disturbances. Structurally, the Stadium Woods has an inverse-J diameter distribution and trees present in all canopy strata. The oldest white oak had periods of asynchronous suppression and release indicating a closed canopy forest with periodic canopy disturbances. The boundary-line release criteria detect a broader range of growth releases, whereas the radial-growth averaging criteria are more specialized for capturing canopy gaps. Release events identified with the boundary-line release criteria lagged an average of 5.8 years behind those identified with the radial-growth averaging criteria because the boundary line release criteria identifies the year of maximum percent growth change, whereas the radial-growth averaging criteria identifies the first year with a detectable increase in radial growth. The Stadium Woods represents a unique collection of unusually large white oak trees growing in a heavily populated area and reveals the importance of long-term tree-ring chronologies stored within urban forest fragments. 
          STUDY NOTES: NOAA Template Raw Measurements file added 2019-02-08.</dc:description>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">NCDC-Paleoclimatology</dc:publisher>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce</dc:publisher>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Copenheaver, C.A.</dc:contributor>
  <dc:date xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">2016-10-05</dc:date>
  <dc:type xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">ONLINE Files</dc:type>
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  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/20795</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/va037.txt</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/northamerica/usa/va037.rwl</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/northamerica/usa/va037-noaa.rwl</dc:identifier>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/va037.txt</dc:source>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/northamerica/usa/va037.rwl</dc:source>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/northamerica/usa/va037-noaa.rwl</dc:source>
  <dc:language xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">English</dc:language>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/20795</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/va037.txt</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/northamerica/usa/va037.rwl</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/northamerica/usa/va037-noaa.rwl</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Carolyn A. Copenheaver, John R. Seiler, John A. Peterson, Andrew M. Evans, Jason L. McVay, Justin H. White2014Stadium Woods: A dendroecological analysis of an old-growth forest fragment on a university campusDendrochronologia32162-7010.1016/j.dendro.2013.09.001http://www.sciencedirect.com/science/article/pii/S1125786513000799</dc:relation>
  <dc:coverage xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">START YEAR: 1697 AD  * END YEAR: 2011 AD</dc:coverage>
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   <ows:LowerCorner>-80.219421  37.222886</ows:LowerCorner>
   <ows:UpperCorner>-80.219421  37.222886</ows:UpperCorner>
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