<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-instrument-1003956</Entry_ID>
  <Entry_Title>Corrientes Instrumental temperature, PAGES LOTRED-SA Version</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Vargas, W.M.; Naumann, G.</Dataset_Creator>
    <Dataset_Title>Corrientes Instrumental temperature, PAGES LOTRED-SA Version</Dataset_Title>
    <Dataset_Release_Date>2013-02-28</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/1003956</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>W.M.</First_Name>
    <Last_Name>Vargas</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>G.</First_Name>
    <Last_Name>Naumann</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>instrumental</Term>
    <Detailed_Variable>collection date,null,null,year Common Era,null,instrumental,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>instrumental</Term>
    <Detailed_Variable>surface air temperature,null,null,degree Celsius,Dec-Feb,instrumental,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>instrumental</Term>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1894 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2004 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>56 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>-27.4</Southernmost_Latitude>
    <Northernmost_Latitude>-27.4</Northernmost_Latitude>
    <Westernmost_Longitude>-58.7</Westernmost_Longitude>
    <Easternmost_Longitude>-58.7</Easternmost_Longitude>
    <Minimum_Altitude>540</Minimum_Altitude>
    <Maximum_Altitude>540</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>South America</Location_Type>
    <Location_Subregion1>Argentina</Location_Subregion1>
    <Detailed_Location>Corrientes&gt;LATITUDE -27.4&gt;LONGITUDE -58.7</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>Neukom, R., J. Luterbacher, R. Villalba, M. Küttel, D. Frank, 
P.D. Jones, M. Grosjean, H. Wanner, J.-C. Aravena, D.E. Black, 
D.A. Christie, R. D&apos;Arrigo, A. Lara, M. Morales, C. Soliz-Gamboa, 
A. Srur, R. Urrutia, and L. von Gunten. 2010.
Multiproxy summer and winter surface air temperature field 
reconstructions for southern South America covering the past centuries. 
Climate Dynamics, Online First March 28, 2010, 
DOI: 10.1007/s00382-010-0793-3
</Reference>
  <Reference>
    <Author>Vargas, W.M.; Naumann, G</Author>
    <Publication_Date>2008</Publication_Date>
    <Title>Impacts of climatic change and low frequency variability in reference series on daily maximum and minimum temperature in southern South America</Title>
    <Volume>8</Volume>
    <Issue>2</Issue>
    <Pages>45-47</Pages>
  </Reference>
  <Summary>
    <Abstract>We statistically reconstruct austral summer (winter) surface air 
temperature fields back to ad 900 (1706) using 22 (20) annually 
resolved predictors from natural and human archives from southern 
South America (SSA). This represents the first regional-scale 
climate field reconstruction for parts of the Southern Hemisphere 
at this high temporal resolution. We apply three different 
reconstruction techniques: multivariate principal component 
regression, composite plus scaling, and regularized expectation 
maximization. There is generally good agreement between the results 
of the three methods on interannual and decadal timescales. 
The field reconstructions allow us to describe differences 
and similarities in the temperature evolution of different 
sub-regions of SSA. The reconstructed SSA mean summer temperatures 
between 900 and 1350 are mostly above the 1901–1995 climatology. 
After 1350, we reconstruct a sharp transition to colder conditions, 
which last until approximately 1700. The summers in the eighteenth 
century are relatively warm with a subsequent cold relapse peaking 
around 1850. In the twentieth century, summer temperatures reach 
conditions similar to earlier warm periods. The winter temperatures 
in the eighteenth and nineteenth centuries were mostly below the 
twentieth century average. The uncertainties of our reconstructions 
are generally largest in the eastern lowlands of SSA, where the 
coverage with proxy data is poorest. Verifications with independent 
summer temperature proxies and instrumental measurements suggest 
that the interannual and multi-decadal variations of SSA temperatures 
are well captured by our reconstructions. This new dataset can be 
used for data/model comparison and data assimilation as well as 
for detection and attribution studies at sub-continental scales. 
 
          STUDY NOTES: Uploaded by R. Neukom, data obtained from original authors.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/reconstructions/pages2k/lotred-sa2k/Corrientes.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>
