<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-lake-13114</Entry_ID>
  <Entry_Title>Ayr Lake, Baffin Island 570Yr Leaf Wax Hydrogen Isotope and Varve Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Thomas, E.K.; McGrane, S.; Briner, J.P.; Huang, Y.</Dataset_Creator>
    <Dataset_Title>Ayr Lake, Baffin Island 570Yr Leaf Wax Hydrogen Isotope and Varve Data</Dataset_Title>
    <Dataset_Release_Date>2012-06-30</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>Pending</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/13114</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.K.</First_Name>
    <Last_Name>Thomas</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>McGrane</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.P.</First_Name>
    <Last_Name>Briner</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Huang</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>sample identification,null,null,null,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C28 n-alkanoic acid,one standard deviation,per mil VSMOW,null,paleolimnology,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C24 n-alkanoic acid,null,per mil VSMOW,null,paleolimnology,averaged,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C30 n-alkanoic acid,null,per mil VSMOW,null,paleolimnology,averaged,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C22 n-alkanoic acid,one standard deviation,per mil VSMOW,null,paleolimnology,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C22 n-alkanoic acid,null,per mil VSMOW,null,paleolimnology,averaged,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C28 n-alkanoic acid,null,per mil VSMOW,null,paleolimnology,averaged,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C26 n-alkanoic acid,one standard deviation,per mil VSMOW,null,paleolimnology,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C24 n-alkanoic acid,one standard deviation,per mil VSMOW,null,paleolimnology,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C26 n-alkanoic acid,null,per mil VSMOW,null,paleolimnology,averaged,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>varve thickness,null,null,millimeter,null,paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Detailed_Variable>delta 2H,C30 n-alkanoic acid,one standard deviation,per mil VSMOW,null,paleolimnology,null,isotope ratio mass spectrometry,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>hydrogen isotopes</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES Arctic 2k</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1433 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2004 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>517 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-54 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>70.459</Southernmost_Latitude>
    <Northernmost_Latitude>70.459</Northernmost_Latitude>
    <Westernmost_Longitude>-70.086</Westernmost_Longitude>
    <Easternmost_Longitude>-70.086</Easternmost_Longitude>
    <Minimum_Altitude>68</Minimum_Altitude>
    <Maximum_Altitude>68</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>Canada</Location_Subregion1>
    <Location_Subregion2>Nunavut</Location_Subregion2>
    <Detailed_Location>Ayr Lake&gt;LATITUDE 70.459&gt;LONGITUDE -70.086</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>Thomas, E.K., S. McGrane, J.P. Briner, and Y. Huang. 2012. 
Leaf wax d2H and varve-thickness climate proxies from 
proglacial lake sediments, Baffin Island, Arctic Canada. 
Journal of Paleolimnology, Vol. 48, No. 1, June 2012, pp. 193-207. 
DOI: 10.1007/s10933-012-9584-7</Reference>
  <Summary>
    <Abstract>We present a multiproxy paleoclimate record using leaf wax hydrogen 
isotopes (d2Hwax) and varve thickness from Arctic proglacial lake 
sediments. We also provide one of the first evaluations of the 
utility of d2Hwax as a paleoclimate proxy in Arctic proglacial lakes. 
We compare varve thickness and d2Hwax at sub-decadal resolution from 
1948 to 2004 AD, and at sub-centennial resolution from 1450 to 2004 AD. 
Varve thickness and d2Hwax both contain large interannual variability 
and are anti-correlated during the late twentieth century, suggesting 
that both proxies respond rapidly, but by different mechanisms, 
to catchment-scale forcings. At longer time scales, varve thickness 
exhibits a strong response to Little Ice Age cooling (1661-1827 AD 
in this record) but does not show evidence for twentieth century 
warming recorded throughout the Arctic. d2Hwax does record regional-
scale temperature changes, with more 2H-depleted values during the 
Little Ice Age and an abrupt change to more 2H-enriched values 
in the twentieth century. This corresponds well with a recent 
Arctic-wide temperature reconstruction in which the seventeenth 
century is the coldest interval, and the twentieth century is the 
warmest interval. Our results suggest that d2Hwax is a promising proxy 
that can be applied at high resolution in proglacial Arctic lakes.  
          STUDY NOTES: Leaf wax hydrogen isotope data (d2Hwax) and varve thickness data 
from sediments collected in proglacial Ayr Lake, eastern Baffin Island, 
Arctic Canada.  

Ayr Lake, Baffin Island: 70.459°N, 70.086°W, 68m elevation, ~50m depth. </Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/canada/baffin/ayr2012.txt</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/canada/baffin/ayr2012.xls</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>
