<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-model-12483</Entry_ID>
  <Entry_Title>LOVECLIM Climate Model Simulation Constrained by Mann et al. 2009 Reconstruction</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Goosse, H.; Crespin, E.; Dubinkina, S.; Loutre, M.F.; Mann, M.E.; Renssen, H.; Sallaz-Damaz, Y.; Shindell, D.</Dataset_Creator>
    <Dataset_Title>LOVECLIM Climate Model Simulation Constrained by Mann et al. 2009 Reconstruction</Dataset_Title>
    <Dataset_Release_Date>2012-02-10</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/12483</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Goosse</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.</First_Name>
    <Last_Name>Crespin</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Dubinkina</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.F.</First_Name>
    <Last_Name>Loutre</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.E.</First_Name>
    <Last_Name>Mann</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>H.</First_Name>
    <Last_Name>Renssen</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Y.</First_Name>
    <Last_Name>Sallaz-Damaz</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>Shindell</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoclimatic modeling</Term>
    <Detailed_Variable>latitude,null,null,degree north,null,paleoclimatic modeling,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoclimatic modeling</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,paleoclimatic modeling,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoclimatic modeling</Term>
    <Detailed_Variable>surface air temperature,null,null,degree Celsius,annual,paleoclimatic modeling,anomalized,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>paleoclimatic modeling</Term>
    <Detailed_Variable>longitude,null,null,degree east,null,paleoclimatic modeling,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>model</Term>
    <Variable_Level_1>atmosphere model</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Medieval Climate Anomaly (MCA)</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>500 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2000 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1450 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-50 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-90</Southernmost_Latitude>
    <Northernmost_Latitude>90</Northernmost_Latitude>
    <Westernmost_Longitude>-180</Westernmost_Longitude>
    <Easternmost_Longitude>180</Easternmost_Longitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Geographic Region</Location_Category>
    <Location_Type>Global</Location_Type>
    <Detailed_Location>Global&gt;LATITUDE &gt;LONGITUDE </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>Goosse, H., E. Crespin, S. Dubinkina, M.F. Loutre, M.E. Mann, 
H. Renssen, Y. Sallaz-Damaz, and D. Shindell.  2012. 
The role of forcing and internal dynamics in explaining 
the &quot;Medieval Climate Anomaly&quot;. 
Climate Dynamics, doi: 10.1007/s00382-012-1297-0</Reference>
  <Summary>
    <Abstract>Proxy reconstructions suggest that peak global temperature 
during the past warm interval known as the Medieval Climate 
Anomaly (MCA, roughly 950-1250 AD) has been exceeded only 
during the most recent decades. To better understand the 
origin of this warm period, we use model simulations 
constrained by data assimilation establishing the spatial 
pattern of temperature changes that is most consistent 
with forcing estimates, model physics and the empirical 
information contained in paleoclimate proxy records. 
These numerical experiments demonstrate that the 
reconstructed spatial temperature pattern of the MCA 
can be explained by a simple thermodynamical response 
of the climate system to relatively weak changes in radiative 
forcing combined with a modification of the atmospheric 
circulation, displaying some similarities with the positive 
phase of the so-called Arctic Oscillation, and with northward 
shifts in the position of the Gulf Stream and Kuroshio currents. 
The mechanisms underlying the MCA are thus quite different 
from anthropogenic mechanisms responsible for modern global 
warming. 

 
          STUDY NOTES: We have performed simulations with the LOVECLIM climate model 
(Goosse et al. 2010) using a so-called &quot;particle filter&quot; 
(van Leeuwen 2009; Dubinkina et al. 2011) that constrains model 
results to follow the signal provided by an annual mean surface 
temperature reconstruction based on a global proxy data network 
(Mann et al. 2009). The central variable in our results is thus 
also the annual mean temperature. The data constrain is applied 
only over the region 30-90°N so this is the only region where 
a good agreement with the reconstruction is expected. 


The data is in the file ts_LOVECLIM_ASSIM_MANN2009.nc. 
It includes annual mean temperatures on a Gaussian 62 x 32 grid. 
The data is in netCDF format and contains one variable, ts, 
the surface temperature in the model in °C for the period 501AD-2000AD. 
It is the best estimate provided by the data assimilation method. 

</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/gcmoutput/goosse2012/ts_loveclim_assim_mann2009.nc</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/gcmoutput/goosse2012/readme-goosse2012.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/gcmoutput/goosse2012/ts_loveclim_assim_mann2009.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>
