<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-loess-12971</Entry_ID>
  <Entry_Title>Chinese Loess Plateau 60KYr Grain Size Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Sun, Y.; Clemens, S.C.; Morrill, C.; Lin, X.P.; Wang, X.L.; An, Z.</Dataset_Creator>
    <Dataset_Title>Chinese Loess Plateau 60KYr Grain Size Data</Dataset_Title>
    <Dataset_Release_Date>2012-05-30</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/12971</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Sun</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.C.</First_Name>
    <Last_Name>Clemens</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.</First_Name>
    <Last_Name>Morrill</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.P.</First_Name>
    <Last_Name>Lin</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>X.L.</First_Name>
    <Last_Name>Wang</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Z.</First_Name>
    <Last_Name>An</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>magnetic susceptibility,loess,null,unspecified unit,null,loess,null,null,N,Gulang</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>depth,null,null,meter,null,loess,null,null,N,Jingyuan</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,loess,null,null,N,Jingyuan OSL age</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>depth,null,null,meter,null,loess,null,null,N,Gulang</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>age,null,null,calendar kiloyear before present,null,loess,null,null,N,Gulang OSL age</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>magnetic susceptibility,loess,null,unspecified unit,null,loess,null,null,N,Jingyuan</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>grain size mean,loess,null,micrometer,null,loess,null,null,N,Jingyuan</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
    <Detailed_Variable>grain size mean,loess,null,micrometer,null,loess,null,null,N,Gulang</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>loess</Term>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Meridional Overturning Circulation (MOC)</Keyword>
  <Keyword>Monsoon</Keyword>
  <Keyword>abrupt climate change</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>60100 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>2000 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>36.35</Southernmost_Latitude>
    <Northernmost_Latitude>37.49</Northernmost_Latitude>
    <Westernmost_Longitude>102.88</Westernmost_Longitude>
    <Easternmost_Longitude>104.6</Easternmost_Longitude>
    <Minimum_Altitude>2210</Minimum_Altitude>
    <Maximum_Altitude>2400</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>China</Location_Subregion2>
    <Detailed_Location>Jingyuan&gt;LATITUDE 36.35&gt;LONGITUDE 104.6</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Asia</Location_Type>
    <Location_Subregion1>Eastern Asia</Location_Subregion1>
    <Location_Subregion2>China</Location_Subregion2>
    <Detailed_Location>Gulang&gt;LATITUDE 37.49&gt;LONGITUDE 102.88</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>Sun, Y.B., S.C. Clemens, C. Morrill, X.P. Lin, X.L. Wang, 
and Z.S. An. 2012. 
Influence of Atlantic meridional overturning circulation 
on the East Asian winter monsoon. 
Nature Geoscience, Vol. 5, pp. 46-49. 
DOI: 10.1038/NGEO1326 </Reference>
  <Summary>
    <Abstract>The last glacial period was characterized by abrupt, millennial-scale 
climate change. These climate fluctuations are particularly pronounced 
in records of the East Asian monsoon system, and seem to be linked to 
changes in North Atlantic circulation. Here we present records of 
grain size variations from the northwestern Chinese Loess Plateau, 
dated using optically stimulated luminescence. We reconstruct changes 
in the strength of the East Asian winter monsoon over the past 60,000 
years and find reconstructed millennial-scale variations that are 
broadly correlated with temperature variations over Greenland, 
suggesting a common forcing. We investigate the effect of a slow-down 
of Atlantic meridional overturning circulation on the monsoon system 
using a coupled climate model simulation with added freshwater flux 
into the northern North Atlantic, and find a strengthening winter 
monsoon circulation over the regions that supply dust to the Loess
Plateau and a reduction in summer monsoon precipitation over East Asia. 
We conclude that Atlantic meridional overturning circulation 
is a driver of abrupt change in the East Asian winter and summer 
monsoon systems, and that the northern westerlies play a role 
in transmitting this signal from the North Atlantic to the Asian 
monsoon regions. 
          STUDY NOTES: Grain size data for the past 60,000 years from 2 loess sections 
in the northwestern Chinese Loess Plateau.  20-m sampling pits 
were excavated at Jingyuan and Gulang, with age models developed 
via 40 optically stimulated luminescence (OSL) measurements. 
Grain size was measured on 2000 samples taken at 2-cm. intervals. 
Grain size data is interpreted as a winter monsoon strength proxy. 

Jingyuan, Chinese Loess Plateau: 36.35°N, 104.6°E,  2210 m elev. 
Gulang, Chinese Loess Plateau:   37.49°N, 102.88°E, 2400 m elev.

</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/loess/china/sun2012clp.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/loess/china/sun2012clp.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>
