<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-recon-10427</Entry_ID>
  <Entry_Title>Lake Silvaplana, Switzerland 1000 Year Chironomid Inferred Temperature</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Larocque, I.; Grosjean, M.; Heiri, O.; Trachsel, M.; Kamenik, C.</Dataset_Creator>
    <Dataset_Title>Lake Silvaplana, Switzerland 1000 Year Chironomid Inferred Temperature</Dataset_Title>
    <Dataset_Release_Date>2010-05-21</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/10427</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>I.</First_Name>
    <Last_Name>Larocque</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Grosjean</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>O.</First_Name>
    <Last_Name>Heiri</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Trachsel</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.</First_Name>
    <Last_Name>Kamenik</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>surface air temperature,midge assemblage,null,degree Celsius,Jul,climate reconstructions|insect|paleolimnology,null,null,N,20-year triangular filter</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|insect|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>surface air temperature,midge assemblage,null,degree Celsius,Jul,climate reconstructions|insect|paleolimnology,null,null,N,3-year triangular filter</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>surface air temperature,midge assemblage,null,degree Celsius,Jul,climate reconstructions|insect|paleolimnology,null,null,N,10-year triangular filter</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|insect|paleolimnology</Term>
    <Detailed_Variable>surface air temperature,midge assemblage,null,degree Celsius,Jul,climate reconstructions|insect|paleolimnology,null,null,N,50-year triangular filter</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>reconstructions</Term>
    <Variable_Level_1>air temperature</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Air Temperature Reconstruction</Keyword>
  <Keyword>Medieval Warm Period</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1032 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1998 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>918 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-48 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>46.45</Southernmost_Latitude>
    <Northernmost_Latitude>46.45</Northernmost_Latitude>
    <Westernmost_Longitude>9.8</Westernmost_Longitude>
    <Easternmost_Longitude>9.8</Easternmost_Longitude>
    <Minimum_Altitude>1800</Minimum_Altitude>
    <Maximum_Altitude>1800</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Europe</Location_Type>
    <Location_Subregion1>Western Europe</Location_Subregion1>
    <Location_Subregion2>Switzerland</Location_Subregion2>
    <Detailed_Location>Lake Silvaplana&gt;LATITUDE 46.45&gt;LONGITUDE 9.8</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>Larocque-Tobler, I., M. Grosjean, O. Heiri, M. Trachsel, 
and C. Kamenik. 2010.
Thousand years of climate change reconstructed from chironomid 
subfossils preserved in varved lake Silvaplana, Engadine, Switzerland. 
Quaternary Science Reviews, Volume 29, Issues 15-16, July 2010, Pages 1940-1949 doi:10.1016/j.quascirev.2010.04.018 
</Reference>
  <Summary>
    <Abstract>Fossil chironomids (non-biting midges) from varved Lake Silvaplana, 
Switzerland, were used to reconstruct climate (mean July air temperatures) 
during the last millennium. At the beginning of the record, corresponding 
to the last part of the &quot;Medieval Climate Anomaly&quot; (MCA) (here the period 
between ca 1032 and 1262 AD), the chironomid-inferred mean July air 
temperatures were 1 °C warmer (p &lt; 0.01) than the climate reference period 
(1961-1990). The &quot;Little Ice Age&quot; seems to have been separated into three 
phases: significantly colder (-1.1 °C in average, p&lt; 0.001) temperatures 
were inferred between ca 1262 and 1481 AD, between ca 1514 and 1718 AD 
(-1.2 °C in average, p&lt; 0.001) and between ca 1734 and 1782 AD (-0.6 °C 
in average, p&lt; 0.1). Although the average temperature changes inferred by
chironomids were within the error of prediction (1.5 °C) of the chironomid-
temperature inference model used for reconstruction, the pattern of 
temperature changes corresponds well with records of the past millennium 
in Switzerland, in Europe and in the Northern Hemisphere. The average 
inferred July temperatures between ca 1900 and 2001 AD were significantly 
warmer (p &lt; 0.05) than the climate reference period (1961-1990) by 1 °C 
which is in agreement with the instrumental data. The inferred July 
temperatures were in the same range as the inferred temperatures during 
the last part of the MCA suggesting that during the 20th century, 
at Lake Silvaplana, the chironomid-inferred temperatures do not
exceed the natural climate variability of the past millennium.
 
          STUDY NOTES: Chironomid-inferred mean July temperature from Lake Silvaplana, 
Switzerland for the last 1000 years. Data are presented with  
3-year, 10-year, 20-year, and 50-year triangular filters, 
as plotted in Figure 6a of Larocque-Tobler et al. 2010. </Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/europe/switzerland/silvaplana2010.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/paleolimnology/europe/switzerland/silvaplana2010.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>
