<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-lake-13016</Entry_ID>
  <Entry_Title>Lake Silvaplana, Switzerland 775 Year Summer Temperature Reconstruction</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Trachsel, M.; Grosjean, M.; Schnyder, D.; Kamenik, C.; Rein, B.</Dataset_Creator>
    <Dataset_Title>Lake Silvaplana, Switzerland 775 Year Summer Temperature Reconstruction</Dataset_Title>
    <Dataset_Release_Date>2012-06-13</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/13016</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Trachsel</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.</First_Name>
    <Last_Name>Grosjean</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Schnyder</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.</First_Name>
    <Last_Name>Kamenik</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.</First_Name>
    <Last_Name>Rein</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|paleolimnology</Term>
    <Detailed_Variable>surface temperature,null,null,degree Celsius,Jun-Aug,climate reconstructions|paleolimnology,filtered,null,N,9-100 year band pass filtered; based on visible reflectance spectroscopy</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>reconstruction</Variable_Level_1>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleolimnology</Term>
    <Variable_Level_1>physical properties</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Air Temperature Reconstruction</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1175 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1949 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>775 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>1 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>Trachsel, M., M. Grosjean, D. Schnyder, C. Kamenik, and B. Rein. 2010. 
Scanning reflectance spectroscopy (380–730 nm): a novel method for 
quantitative high-resolution climate reconstructions from minerogenic 
lake sediments. 
Journal of Paleolimnology, December 2010, Vol. 44, Issue 4, pp 979-994. 
DOI: 10.1007/s10933-010-9468-7 </Reference>
  <Summary>
    <Abstract>High-resolution (annual to sub-decadal) quantitative reconstructions 
of climate variables are needed from a variety of paleoclimate archives 
across the world to place current climate change in the context of 
long-term natural climate variability.  Rapid, high-resolution, 
non-destructive scanning techniques are required to produce such 
high-resolution records from lake sediments. In this study we explored 
the potential of scanning reflectance spectroscopy (VIS-RS; 380-730 nm) 
to produce quantitative summer temperature reconstructions from 
minerogenic sediments of proglacial, annually laminated Lake Silvaplana, 
in the eastern Swiss Alps. The scanning resolution was 2 mm, 
which corresponded to sediment deposition over 1-2 years. We found 
correlations up to r = 0.84 (p&lt;0.05) for the calibration period 
1864-1950, between six reflectance-dependent variables and summer 
(JJAS) temperature. These reflectance-dependent variables (e.g. slope 
of the reflectance 570/630 nm, indicative of illite, biotite 
and chlorite; minimum reflectance at 690 nm indicative of chlorite) 
indicate the mineralogical composition of the clastic sediments, 
which is, in turn, related to climate in the catchment of this 
particular proglacial lake. We used multiple linear regression (MLR) 
to establish a calibration model that explains 84% of the variance 
of summer (JJAS) temperature during the calibration period 1864-1950. 
We then applied the calibration model downcore to develop a 
quantitative summer temperature reconstruction extending back to 
AD 1177. This temperature reconstruction is in good agreement with 
two independent temperature reconstructions based on documentary data 
that extend back to AD 1500 and tree ring data that extend back to 
AD 1177. This study confirms the great potential of in situ scanning 
reflectance spectroscopy as a novel non-destructive technique to 
rapidly acquire high-resolution quantitative paleoclimate information 
from minerogenic lake sediments. 

 
          STUDY NOTES: 775 year summer (JJA) temperature reconstruction for the Swiss Alps 
based on  visible reflectance spectroscopy from Lake Silvaplana, 
Switzerland. 

Lake Silvaplana, Switzerland: 46°27&apos;N, 9°48&apos;E, 1800m </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/silvaplana2010c.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/paleolimnology/europe/switzerland/silvaplana2010c.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>
