<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-icecore-9898</Entry_ID>
  <Entry_Title>EPICA Dronning Maud Land Ice Core 64-30KYr CO2 Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Lüthi, D.; Bereiter, B.; Stauffer, B.; Winkler, R.; Schwander, J.; Kindler, P.; Leuenberger, M.; Kipfstuhl, S.; Capron, E.; Landais, A.; Fischer, H.; Stocker, T.F.</Dataset_Creator>
    <Dataset_Title>EPICA Dronning Maud Land Ice Core 64-30KYr CO2 Data</Dataset_Title>
    <Dataset_Release_Date>2010-10-04</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/9898</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Lüthi</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Bereiter</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Stauffer</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.</First_Name>
    <Last_Name>Winkler</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Schwander</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.</First_Name>
    <Last_Name>Kindler</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Leuenberger</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Kipfstuhl</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.</First_Name>
    <Last_Name>Capron</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Landais</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Fischer</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>T.F.</First_Name>
    <Last_Name>Stocker</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate forcing|ice cores</Term>
    <Detailed_Variable>carbon dioxide,bulk atmosphere,one standard deviation,parts per million,null,climate forcing|ice cores,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate forcing|ice cores</Term>
    <Detailed_Variable>carbon dioxide,bulk atmosphere,null,parts per million,null,climate forcing|ice cores,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>depth,null,null,meter,null,ice cores,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>gas age,null,null,calendar year before present,null,ice cores,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice core</Term>
    <Variable_Level_1>atmospheric gas</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>carbon cycle</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>63750 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>30775 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-75</Southernmost_Latitude>
    <Northernmost_Latitude>-75</Northernmost_Latitude>
    <Westernmost_Longitude>.07</Westernmost_Longitude>
    <Easternmost_Longitude>.07</Easternmost_Longitude>
    <Minimum_Altitude>2892</Minimum_Altitude>
    <Maximum_Altitude>2892</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Antarctica</Location_Type>
    <Detailed_Location>EPICA Dronning Maud Land&gt;LATITUDE -75&gt;LONGITUDE .07</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>Lüthi, D., B. Bereiter, B. Stauffer, R. Winkler, J. Schwander,
P. Kindler, M. Leuenberger, S. Kipfstuhl, E. Capron, A. Landais,
H. Fischer, and T.F. Stocker. 2010.
CO2 and O2/N2 variations in and just below the bubble-clathrate 
transformation zone of Antarctic ice cores. 
Earth and Planetary Science Letters, Vol. 297, pp. 226-233.  
doi:10.1016/j.epsl.2010.06.023  
</Reference>
  <Summary>
    <Abstract>CO2 measurements on the EPICA (European Project for Ice Coring 
in Antarctica) DML ice core in depth levels just below the bubble 
ice-clathrate ice transformation zone (1230-2240 m depth) were 
performed. In the youngest part (1230-1600 m), they reveal 
variations of up to 25 ppmv around the mean atmospheric 
concentration within centimetres, corresponding to a snow 
deposition interval of a few years. Similar results are found 
at corresponding depth regions of the Dome C and the Talos Dome 
ice cores. Since we can exclude all hitherto known processes 
altering the concentration of CO2 in ice cores, we present 
a hypothesis about spatial fractionation of air components 
related to episodically increasing clathrate formation followed 
by diffusion processes from bubbles to clathrates. This hypothesis 
is supported by optical line-scan observations and by O2/N2 
measurements at the same depth where strong CO2 variations are 
detected. Below the clathrate formation zone, this small-scale 
fractionation process is slowly smoothed out, most likely by 
diffusion, regaining the initial mean atmospheric concentration. 
Although this process compromises the representativeness of a 
single CO2 measurement on small ice samples in the clathrate 
formation zone of an ice core, it does not affect the mean 
atmospheric CO2 concentration if CO2 values are averaged over 
a sufficiently long depth scale (&gt;10 cm in case of the EPICA 
DML ice core).
 
          STUDY NOTES: CO2 record from the EPICA Dronning Maud Land ice core covering 
the time period between 64000 and 30000 yr BP. 

</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/maud/edml-co2-64-30ka.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/icecore/antarctica/maud/edml-co2-64-30ka.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>2019-05-06</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-05-06</Last_DIF_Revision_Date>
</DIF>
