<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-5465</Entry_ID>
  <Entry_Title>Baffin Island 500 Year Summer Temperature Reconstruction</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Hughen, K.A.; Overpeck, J.T.; Anderson, R.F.</Dataset_Creator>
    <Dataset_Title>Baffin Island 500 Year Summer Temperature Reconstruction</Dataset_Title>
    <Dataset_Release_Date>2003-10-01</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/5465</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>K.A.</First_Name>
    <Last_Name>Hughen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.T.</First_Name>
    <Last_Name>Overpeck</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.F.</First_Name>
    <Last_Name>Anderson</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>surface air temperature,varve thickness,null,degree Celsius,Jun,climate reconstructions|paleolimnology,null,null,N,based on varve thickness</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|paleolimnology,null,null,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,dark laminae</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>reconstruction</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Air Temperature Reconstruction</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>436 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-42 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>62.9167</Southernmost_Latitude>
    <Northernmost_Latitude>62.9167</Northernmost_Latitude>
    <Westernmost_Longitude>-69.8833</Westernmost_Longitude>
    <Easternmost_Longitude>-69.8833</Easternmost_Longitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>Canada</Location_Subregion1>
    <Location_Subregion2>Northwest Territories</Location_Subregion2>
    <Detailed_Location>Upper Soper Lake&gt;LATITUDE 62.9167&gt;LONGITUDE -69.8833</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>Hughen, K.A., J.T. Overpeck, R.F. Anderson. 2000. Recent Warming in a 500-Year Paleotemperature Record from Varved Sediments: Upper Soper Lake, Baffin Island, Canada. The Holocene Vol. 10, no. 1, pp. 9-19</Reference>
  <Summary>
    <Abstract>Laminated sediments from Upper Soper Lake on southern Baffin Island  provide a new 500-year record of temperature change in the Arctic.  Radiometric dating, using 210 Pb and Pu, shows that the light- and  dark-coloured laminae couplets are annually deposited varves.  Dark laminae thickness is strongly correlated to average June temperature  from Kimmirut (r = 0.82), reflecting the influence of temperature on  snowmelt and fluxes of runoff and suspended sediment. This relationship  allowed the construction of a palaeotemperature record that documents  large-amplitude interannual to decadal variability superimposed on  distinct century-scale trends, including 2°C average warming and maximum  temperatures during the 1900s. Similar patterns of change are seen in  individual and regionally averaged palaeotemperature records from around  the circum-Arctic. Upper Soper Lake records temperatures, rates of change  and variance during the twentieth century that are all anomalously high  within the context of the last 500 years, and outside the observed range  of natural variability. Comparisons of Upper Soper Lake and Arctic average  palaeotemperature to proxy-records of hypothesized forcing mechanisms  suggest that the recent warming trend is mostly due to anthropogenic  emissions of atmospheric greenhouse gases. The magnitude of the warming  and decade-scale variability throughout the records, however, indicate  that natural forcing mechanisms such as changing solar irradiance and  volcanic activity, as well as positive feedbacks within the Arctic  environment, also play an important role. 
          STUDY NOTES: Summer temperature reconstruction based on laminae thickness in sediments from Upper Soper Lake, Baffin Island, Canada.</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/soper_2000.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>
