<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-13218</Entry_ID>
  <Entry_Title>Lake Braya Sø, Greenland 7,000 Year Temperature Reconstructions</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>von Gunten, L.; D&apos;Andrea, W.J.; Bradley, R.S.; Huang, Y.</Dataset_Creator>
    <Dataset_Title>Lake Braya Sø, Greenland 7,000 Year Temperature Reconstructions</Dataset_Title>
    <Dataset_Release_Date>2012-08-29</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/13218</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>von Gunten</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>W.J.</First_Name>
    <Last_Name>D&apos;Andrea</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.S.</First_Name>
    <Last_Name>Bradley</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>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>lake surface temperature,alkenone unsaturation index,unspecified error upper bound,degree Celsius,null,climate reconstructions|paleolimnology,null,null,N,based on Uk37 and VIS-RS</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>lake surface temperature,alkenone unsaturation index,unspecified error lower bound,degree Celsius,null,climate reconstructions|paleolimnology,null,null,N,based on Uk37 and VIS-RS</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>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>lake surface temperature,alkenone unsaturation index,null,degree Celsius,null,climate reconstructions|paleolimnology,filtered|interpolated,null,N,based on Uk37 and VIS-RS; linearly interpolated to annual time steps; band-pass filtered 50-70 years</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>lake surface temperature,alkenone unsaturation index,null,degree Celsius,null,climate reconstructions|paleolimnology,null,null,N,based on Uk37 and VIS-RS</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>reconstruction</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Air Temperature Reconstruction</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>-4999 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2005 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>6949 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-55 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>69.9875</Southernmost_Latitude>
    <Northernmost_Latitude>69.9875</Northernmost_Latitude>
    <Westernmost_Longitude>-51.0333</Westernmost_Longitude>
    <Easternmost_Longitude>-51.0333</Easternmost_Longitude>
    <Minimum_Altitude>170</Minimum_Altitude>
    <Maximum_Altitude>170</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>Greenland</Location_Subregion1>
    <Detailed_Location>Lake Braya Sø&gt;LATITUDE 69.9875&gt;LONGITUDE -51.0333</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>von Gunten, L., W.J. D&apos;Andrea, R.S. Bradley, and Y. Huang. 2012. 
Proxy-to-proxy calibration: Increasing the temporal resolution 
of quantitative climate reconstructions. 
Scientific Reports 2, Article number 609, 29 August 2012. 
doi:10.1038/srep00609 </Reference>
  <Summary>
    <Abstract>High-resolution paleoclimate reconstructions are often restricted 
by the difficulties of sampling geologic archives in great detail 
and the analytical costs of processing large numbers of samples. 
Using sediments from Lake Braya Sø, Greenland, we introduce a new 
method that provides a quantitative high-resolution paleoclimate 
record by combining measurements of the alkenone unsaturation index 
(UK37) with non-destructive scanning reflectance spectroscopic 
measurements in the visible range (VIS-RS). The proxy-to-proxy (PTP) 
method exploits two distinct calibrations: the in situ calibration 
of UK37 to lake water temperature and the calibration of scanning 
VIS-RS data to down core UK37 data. Using this approach, we produced 
a quantitative temperature record that is longer and has 5 times 
higher sampling resolution than the original UK37 time series, 
thereby allowing detection of temperature variability in frequency 
bands characteristic of the AMO over the past 7,000 years.
 
          STUDY NOTES: High-resolution temperature reconstructions based on alkenone data 
and scanning reflectance spectroscopy measurements from sediments 
collected in Lake Braya Sø, West Greenland.  Free lipids were 
extracted from core BS01-01, freeze-dried and homogenized.  
Alkenone samples at 0.5 cm intervals were quantified by 
gas-chromatography-flame-ionization-detection. The VIS-RS 
measurements were conducted on an overlapping core (BS03-01) 
at 2mm intervals.  Relative Absorption Band Depth at 660-760 nm 
was utilized for the reconstructions. 

Lake Braya Sø, West Greenland: 66°59&apos;15&quot;N, 51°02&apos;0&quot;W, 170m elev, 24m 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/greenland/braya-so2012.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/greenland/braya-so2012.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>
