<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-12995</Entry_ID>
  <Entry_Title>EDML-Talos Dome Antarctic Ice Core 38-115KYrBP CO2 Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Bereiter, B.; Lüthi, D.; Siegrist, M.; Schüpbach, S.; Stocker, T.F.; Fischer, H.</Dataset_Creator>
    <Dataset_Title>EDML-Talos Dome Antarctic Ice Core 38-115KYrBP CO2 Data</Dataset_Title>
    <Dataset_Release_Date>2012-06-11</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/12995</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Bereiter</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Lüthi</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Siegrist</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Schüpbach</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>T.F.</First_Name>
    <Last_Name>Stocker</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Fischer</Last_Name>
  </Personnel>
  <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,EDML1_Sc4 gas age</Detailed_Variable>
  </Parameters>
  <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>ice cores</Term>
    <Detailed_Variable>notes,null,null,null,null,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,TALDICE-1a gas age</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,averaged,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>Meridional Overturning Circulation (MOC)</Keyword>
  <Keyword>carbon cycle</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>114193 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>34167 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>-72.8166</Northernmost_Latitude>
    <Westernmost_Longitude>.07</Westernmost_Longitude>
    <Easternmost_Longitude>159.1833</Easternmost_Longitude>
    <Minimum_Altitude>2315</Minimum_Altitude>
    <Maximum_Altitude>2892</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Antarctica</Location_Type>
    <Detailed_Location>Talos Dome TALDICE&gt;LATITUDE -72.8166&gt;LONGITUDE 159.1833</Detailed_Location>
  </Location>
  <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>Bereiter, B., D. Lüthi, M. Siegrist, S. Schüpbach, T.F. Stocker, 
and H. Fischer. 2012. 
Mode change of millennial CO2 variability during the last 
glacial cycle associated with a bipolar marine carbon seesaw. 
Proceedings of the National Academy of Sciences, 
published ahead of print June 6, 2012, 
doi:10.1073/pnas.1204069109 </Reference>
  <Summary>
    <Abstract>Important elements of natural climate variations during the last 
ice age are abrupt temperature increases over Greenland and related 
warming and cooling periods over Antarctica. Records from Antarctic 
ice cores have shown that the global carbon cycle also plays a 
role in these changes. The available data shows that atmospheric 
CO2 follows closely temperatures reconstructed from Antarctic ice 
cores during these variations. Here, we present new high-resolution 
CO2 data from Antarctic ice cores, which cover the period between 
115,000 and 38,000 y before present. Our measurements show that also 
smaller Antarctic warming events have an imprint in CO2 concentrations. 
Moreover, they indicate that during Marine Isotope Stage (MIS) 5, 
the peak of millennial CO2 variations lags the onset of Dansgaard/
Oeschger warmings by 250 +/- 190 y. During MIS 3, this lag increases 
significantly to 870 +/- 90 y. Considerations of the ocean circulation 
suggest that the millennial variability associated with the Atlantic 
Meridional Overturning Circulation (AMOC) undergoes a mode change 
from MIS 5 to MIS 4 and 3. Ocean carbon inventory estimates imply 
that during MIS 3 additional carbon is derived from an extended mass 
of carbon-enriched Antarctic Bottom Water. The absence of such a 
carbon-enriched water mass in the North Atlantic during MIS 5 can 
explain the smaller amount of carbon released to the atmosphere 
after the Antarctic temperature maximum and, hence, the shorter lag. 
Our new data provides further constraints for transient coupled 
carbon cycle-climate simulations during the entire last glacial cycle.  
          STUDY NOTES: High-resolution Carbon Dioxide (CO2) data from two Antarctic ice cores, 
covering the period between 115,000 and 38,000 years before present. 

EPICA Dronning Maud Land Ice Core: 75°00&apos;S,  00°04&apos;E, 2892 m elevation 
TALDICE Talos Dome Ice Core:       72°49&apos;S, 159°11&apos;E, 2315 m elevation </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/edml-talos2012co2.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/edml-talos2012co2.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>
