<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-11818</Entry_ID>
  <Entry_Title>Guoqu Glacier Ice Core, Tibet 70 Year Major Ions Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Grigholm, B.; Mayewski, P.A.; Kang, S.; Zhang, Y.; Kaspari, S.; Sneed, S.; Zhang, Q.</Dataset_Creator>
    <Dataset_Title>Guoqu Glacier Ice Core, Tibet 70 Year Major Ions Data</Dataset_Title>
    <Dataset_Release_Date>2011-07-12</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/11818</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Grigholm</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.A.</First_Name>
    <Last_Name>Mayewski</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Kang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Zhang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Kaspari</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Sneed</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Q.</First_Name>
    <Last_Name>Zhang</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>ice age,null,null,year Common Era,null,ice cores,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>calcium,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>chloride,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>potassium,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>sodium,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</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>nitrate,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>magnesium,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice cores</Term>
    <Detailed_Variable>sulfate,bulk ice,null,microgram per liter,null,ice cores,null,null,N,median</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>ice core</Term>
    <Variable_Level_1>chemistry</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1935 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2004 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>15 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-54 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>33.5772</Southernmost_Latitude>
    <Northernmost_Latitude>33.5772</Northernmost_Latitude>
    <Westernmost_Longitude>91.1765</Westernmost_Longitude>
    <Easternmost_Longitude>91.1765</Easternmost_Longitude>
    <Minimum_Altitude>5720</Minimum_Altitude>
    <Maximum_Altitude>5720</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Detailed_Location>Guoqu Glacier&gt;LATITUDE 33.5772&gt;LONGITUDE 91.1765</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>Grigholm, B., P.A. Mayewski, S. Kang, Y. Zhang, S. Kaspari, 
S.B. Sneed, and Q. Zhang.  2009. 
Atmospheric soluble dust records from a Tibetan ice core: 
Possible climate proxies and teleconnection with the 
Pacific Decadal Oscillation. 
Journal of Geophysical Research, 114, D20118, 
doi:10.1029/2008JD011242</Reference>
  <Summary>
    <Abstract>In autumn 2005, a joint expedition between the University of Maine 
and the Institute of Tibetan Plateau Research recovered three ice 
cores from Guoqu Glacier (33°34&apos;37.8&quot;N, 91°10&apos;35.3&quot;E, 5720 m above 
sea level) on the northern side of Mt. Geladaindong, central Tibetan 
Plateau.  Isotopes (d18O), major soluble ions (Na+, K+, Mg2+, Ca2+, 
Cl-, NO3-,SO4 2-), and radionuclide (b-activity) measurements from 
one of the cores revealed a 70-year record (1935–2005). Statistical 
analysis of major ion time series suggests that atmospheric soluble 
dust species dominate the chemical signature and that background dust 
levels conceal marine ion species deposition. The soluble dust time 
series have interspecies relations and common structure (empirical 
orthogonal function (EOF) 1), suggesting a similar soluble dust 
source or transport route. Annual and seasonal correlations between 
the EOF 1 time series and National Centers for Environmental 
Prediction/National Center for Atmospheric Research reanalysis 
climate variables (1948–2004) suggest that the Mt. Geladaindong 
ice core record provides a proxy for local and regional surface 
pressure. An approximately threefold decrease of soluble dust 
concentrations in the middle to late 1970s, accompanied by regional 
increases in pressure and temperature and decreases in wind velocity, 
coincides with the major 1976-1977 shift of the Pacific Decadal 
Oscillation (PDO) from a negative to a positive state. This is 
the first ice core evidence of a potential teleconnection between 
central Asian atmospheric soluble dust loading and the PDO. 
Analysis of temporally longer ice cores from Mt. Geladaindong 
may enhance understanding of the relationship between the PDO 
and central Asian atmospheric circulation and subsequent 
atmospheric soluble dust loading. 
 
          STUDY NOTES: High resolution (Annual Median Concentrations) Na+, K+, Mg2+, 
Ca2+, Cl-,NO3-, SO42- from the 2005 Guoqu Glacier ice core 
from northern side of Mt. Geladaindong, central Tibetan Plateau. </Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/trop/guoqu/guoqu2009.xls</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/trop/guoqu/guoqu2009.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>
