<DIF xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.8.4.xsd">
  <Entry_ID>noaa-tree-1000093</Entry_ID>
  <Entry_Title>Speer - Experimental Forest - PIPO - OR049, PAGES North America 2K Version</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Speer, J.H.; Swetnam, T.W.</Dataset_Creator>
    <Dataset_Title>Speer - Experimental Forest - PIPO - OR049, PAGES North America 2K Version</Dataset_Title>
    <Dataset_Release_Date>2013-04-10</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>10.7289/V5M9070P</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/1000093</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.H.</First_Name>
    <Last_Name>Speer</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>T.W.</First_Name>
    <Last_Name>Swetnam</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree-ring</Term>
    <Variable_Level_1>width</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES NAmerica 2k</Keyword>
  <Keyword>PIPO</Keyword>
  <Keyword>Pinus ponderosa Douglas ex C. Lawson</Keyword>
  <Keyword>ponderosa pine</Keyword>
  <Keyword>western yellow pine</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1500 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1980 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>450 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-30 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>43.72</Southernmost_Latitude>
    <Northernmost_Latitude>43.72</Northernmost_Latitude>
    <Westernmost_Longitude>-121.6</Westernmost_Longitude>
    <Easternmost_Longitude>-121.6</Easternmost_Longitude>
    <Minimum_Altitude>1530</Minimum_Altitude>
    <Maximum_Altitude>1530</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Oregon</Location_Subregion2>
    <Detailed_Location>Experimental Forest&gt;LATITUDE 43.72&gt;LONGITUDE -121.6</Detailed_Location>
  </Location>
  <Access_Constraints>None</Access_Constraints>
  <Use_Constraints>Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.</Use_Constraints>
  <Data_Set_Language>English</Data_Set_Language>
  <Data_Center>
    <Data_Center_Name>
      <Short_Name>DOC/NOAA/NESDIS/NCEI</Short_Name>
      <Long_Name>National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce </Long_Name>
    </Data_Center_Name>
    <Data_Center_URL>https://www.ncdc.noaa.gov/data-access/paleoclimatology-data</Data_Center_URL>
    <Personnel>
      <Role>DATA Center Contact</Role>
      <First_Name>Bruce</First_Name>
      <Last_Name>Bauer</Last_Name>
      <Email>bruce.a.bauer@noaa.gov</Email>
      <Email>paleo@noaa.gov</Email>
      <Phone>303-497-6280</Phone>
      <Fax>303-497-6513</Fax>
      <Contact_Address>
        <Address>325 Broadway, E/NE31</Address>
        <City>Boulder</City>
        <Province_or_State>CO</Province_or_State>
        <Postal_Code>80305-3328</Postal_Code>
        <Country>USA</Country>
      </Contact_Address>
    </Personnel>
  </Data_Center>
  <Distribution>
    <Distribution_Media>online</Distribution_Media>
    <Distribution_Format>ASCII</Distribution_Format>
  </Distribution>
  <Reference>Speer, J.H., T.W. Swetnam, B.E. Wickman, and A. Youngblood. 2001. Changes in pandora moth outbreak dynamics during the past 622 years. Ecology, 82(3): 679-697.</Reference>
  <Summary>
    <Abstract>Episodic outbreaks of pandora moth (Coloradia pandora Blake), a forest insect that defoliates ponderosa pine (Pinus ponderosa Dougl. ex Laws.) and other pine species in the western United States, have recurred several times during the 20th century in forests of south-central Oregon. We collected and analyzed tree-ring samples from stands affected by recent outbreaks of pandora moth to develop a long-term record of outbreaks.
Outbreaks were evident in tree-ring series as a characteristic ‘‘signature’’ of sharply reduced latewood width within a ring, followed by reduced ring widths lasting 4–20 yr. We verified
that this tree-ring signature was unrelated to drought or other climatic fluctuations by comparing the timing of known and inferred outbreaks with independent climatic data. Using the pandora moth tree-ring signature, we reconstructed a 622-year record of 22
individual outbreaks in 14 old-growth ponderosa pine stands. This is currently the longest
regional reconstruction of forest insect outbreak history in North America. Intervals between
pandora moth outbreaks were highly variable within individual forest stands, ranging from
9 yr to 156 yr. Spectral analyses of a composite time series from all stands, however, showed
more consistent intervals between outbreaks, suggesting quasicyclical population dynamics
at regional and decadal scales. Waveforms extracted from the regional outbreak time series
had periods ranging over ;18–24 yr (39.7% variance explained) and ;37–41 yr (37.3% variance explained). The periods and strengths of these cycles varied across the centuries, with the largest outbreaks occurring when relatively high-amplitude periods of the dominant cycles were in phase. Twentieth-century outbreaks were not more synchronous (extensive), severe, or longer in duration than outbreaks in previous centuries, but there was an unusual 60-yr reduction in regional activity during ;1920–1980. The changing dynamical behavior of pandora moth populations highlights the need to evaluate historical factors that may have influenced this system, such as climatic variations, forest fires, and human land uses.
Although cyclical dynamics in animal populations have most commonly been attributed to endogenous, ecological processes (e.g., ‘‘delayed density dependence,’’ predators, pathogens, and parasites) our findings suggest that exogenous processes (e.g., climatic oscillations) may also be involved.
</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/reconstructions/pages2k/namerica2k/nam-tr_120-or049-1500-1980.txt</URL>
  </Related_URL>
  <IDN_Node>
    <Short_Name>USA/NOAA</Short_Name>
  </IDN_Node>
  <Metadata_Name>DIF</Metadata_Name>
  <Metadata_Version>Version 9.8.4</Metadata_Version>
  <DIF_Creation_Date>2019-02-15</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-02-15</Last_DIF_Revision_Date>
</DIF>
