<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-1003400</Entry_ID>
  <Entry_Title>French Alps, 969 - 2007 AD, tree ring width, Larch, PAGES Euro-Med 2k Version</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Büntgen, U.; Frank, D.C.; Neuenschwander, T.; Esper, J.</Dataset_Creator>
    <Dataset_Title>French Alps, 969 - 2007 AD, tree ring width, Larch, PAGES Euro-Med 2k Version</Dataset_Title>
    <Dataset_Release_Date>2013-05-15</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>10.25921/xagb-9m93</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/1003400</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>U.</First_Name>
    <Last_Name>Büntgen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.C.</First_Name>
    <Last_Name>Frank</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>T.</First_Name>
    <Last_Name>Neuenschwander</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Esper</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree-ring</Term>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES Euro-Med 2k</Keyword>
  <Keyword>LADE</Keyword>
  <Keyword>Larix decidua Mill.</Keyword>
  <Keyword>European larch</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>969 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2007 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>981 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-57 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>44</Southernmost_Latitude>
    <Northernmost_Latitude>44</Northernmost_Latitude>
    <Westernmost_Longitude>7.5</Westernmost_Longitude>
    <Easternmost_Longitude>7.5</Easternmost_Longitude>
    <Minimum_Altitude>2100</Minimum_Altitude>
    <Maximum_Altitude>2100</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Europe</Location_Type>
    <Location_Subregion1>Western Europe</Location_Subregion1>
    <Detailed_Location>Maritime French Alps&gt;LATITUDE 44&gt;LONGITUDE 7.5</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>
    <Author>Büntgen, U., D. Frank, T. Neuenschwander and J. Esper</Author>
    <Publication_Date>2012</Publication_Date>
    <Title>Fading temperature sensitivity of Alpine tree growth at its Mediterranean margin and associated effects on large-scale climate reconstructions</Title>
    <Series>Climatic Change</Series>
    <Volume>114</Volume>
    <Pages>651-666</Pages>
    <DOI>10.1007/s10584-012-0450-4</DOI>
  </Reference>
  <Summary>
    <Abstract>A millennium-long tree-ring width chronology of living and dead larch (Larix decidua Mill.) specimens from the Maritime French Alps was introduced 35 years ago. This
       record has been included in various large-scale temperature reconstructions, though recent analyses revealed only weak associations with regional summer temperatures. Calibration
       and verification trials against instrumental measurements were, however, limited by the original record’s early ending in 1974. Here we introduce an update of this widely considered
       chronology until 2007 and back into medieval times. A total of 297 new larch samples from high-elevation settings in the southern French Alps were included, and the combined
       398 measurement series allowed effects of tree-ring detrending and chronology development to be explored. Comparisons with meteorological temperature, precipitation and drought
       indices revealed weak and temporally inconsistent climate sensitivity. To further place these local findings in a biogeographic context, we used &gt;3,000 larch trees from 61 locations
       across the Alpine arc. This unique network approach confirmed fading temperature sensitivity with decreasing latitude, and thus questioned the overall reliability of ring width-based
       temperature reconstructions in the Mediterranean region. Our results further emphasize the pending need to develop chronologies from maximum latewood densities and stable isotope
       ratios across the lower latitudes, and to carefully evaluate ecological site conditions and methodological data restrictions prior to compiling local data into global networks. 
          STUDY NOTES:   Increment cores from a total of 297 living and dead European larch (Larix decidua Mill.) trees were newly collected at three sites (1, 2, 3) within the same ecological context as the original site 4 (Serre 1978). 
       A unique network &gt;3000 TRW series from 61 locations distributed over the Austrian, Swiss, Slovenian, Italian, and French Alps (see Büntgen et al. 2008a for details) was utilized
       for an Alpine-wide comparison of larch growth responses to variations in summer temperature. The geographical mean of this exceptional Alpine-wide collection is centered
       over the Italian Dolomites (46.63 °N, 11.86 °E and 1,667 m asl).
</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/euro-med2k/Buentgen_et_al_CC_2012.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>2018-12-11</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2018-12-11</Last_DIF_Revision_Date>
</DIF>
