<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-13398</Entry_ID>
  <Entry_Title>NGRIP and EDML Ice Core 32-11KYrBP Methane Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Baumgartner, M.; Schilt, A.; Eicher, O.; Schmitt, J.; Schwander, J.; Spahni, R.; Fischer, H.; Stocker, T.F.</Dataset_Creator>
    <Dataset_Title>NGRIP and EDML Ice Core 32-11KYrBP Methane Data</Dataset_Title>
    <Dataset_Release_Date>2012-10-17</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/13398</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Baumgartner</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Schilt</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>O.</First_Name>
    <Last_Name>Eicher</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Schmitt</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Schwander</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.</First_Name>
    <Last_Name>Spahni</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>ice cores</Term>
    <Detailed_Variable>notes,null,null,null,null,ice cores,null,null,C,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate forcing|ice cores</Term>
    <Detailed_Variable>methane,bulk atmosphere,one standard deviation,parts per billion,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>climate forcing|ice cores</Term>
    <Detailed_Variable>methane,bulk atmosphere,null,parts per billion,null,climate forcing|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>Last Glacial Maximum</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>31924 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>11067 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>75.1</Northernmost_Latitude>
    <Westernmost_Longitude>-42.33</Westernmost_Longitude>
    <Easternmost_Longitude>.07</Easternmost_Longitude>
    <Minimum_Altitude>2892</Minimum_Altitude>
    <Maximum_Altitude>2917</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>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>Greenland</Location_Subregion1>
    <Detailed_Location>NGRIP&gt;LATITUDE 75.1&gt;LONGITUDE -42.33</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>Baumgartner, M., A. Schilt, O. Eicher, J. Schmitt, 
J. Schwander, R. Spahni, H. Fischer and T.F. Stocker. 2012. 
High-resolution interpolar difference of atmospheric methane 
around the Last Glacial Maximum. 
Biogeosciences, Vol. 9, pp. 3961-3977. 
doi:10.5194/bg-9-3961-2012</Reference>
  <Summary>
    <Abstract>Reconstructions of past atmospheric methane concentrations
are available from ice cores from both Greenland
and Antarctica. The difference observed between the two polar
methane concentration levels represents a valuable constraint
on the geographical location of the methane sources.
Here we present new high-resolution methane records from
the North Greenland Ice Core Project (NGRIP) and the European
Project for Ice Coring in Antarctica (EPICA) Dronning
Maud Land (EDML) ice cores covering Termination 1,
the Last Glacial Maximum, and parts of the last glacial back
to 32 000 years before present. Due to the high resolution of
the records, the synchronisation between the ice cores from
NGRIP and EDML is considerably improved, and the interpolar
concentration difference of methane is determined with
unprecedented precision and temporal resolution. Relative
to the mean methane concentration, we find a rather stable
positive relative interpolar difference throughout the record
with its minimum value of 3.7±0.7% between 21 900–
21 200 years before present, which is higher than previously
estimated in this interval close to the Last Glacial Maximum.
This implies that Northern Hemisphere boreal wetland
sources were never completely shut off during the peak
glacial, as suggested from previous bipolar methane concentration
records. Starting at 21 000 years before present, i.e.
several millennia prior to the transition into the Holocene,
the relative interpolar difference becomes even more positive
and stays at a fairly stable level of 6.5±0.8% during
Termination 1. We thus find that the boreal and tropical
methane sources increased by approximately the same factor
during Termination 1. We hypothesise that latitudinal shifts
in the Intertropical Convergence Zone (ITCZ) and the monsoon
system contribute, either by dislocation of the methane
source regions or, in case of the ITCZ, also by changing the
relative atmospheric volumes of the Northern and Southern
Hemispheres, to the subtle variations in the relative interpolar
concentration difference on glacial/interglacial as well as
on millennial time scales. 
          STUDY NOTES: Methane (CH4) record from the EPICA Dronning Maud Land ice core, Antarctica, and the North Greenland Ice Sheet Project (NGRIP) ice core, Greenland, covering 32-11KYrBP.</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/edml2012ch4.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/greenland/summit/ngrip/gases/ngrip2012ch4.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>
