<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-forcing-13136</Entry_ID>
  <Entry_Title>LOSCAR Model Paleocene-Eocene Thermal Maximum pCO2 Output</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Zeebe, R.E.</Dataset_Creator>
    <Dataset_Title>LOSCAR Model Paleocene-Eocene Thermal Maximum pCO2 Output</Dataset_Title>
    <Dataset_Release_Date>2012-07-11</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/13136</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.E.</First_Name>
    <Last_Name>Zeebe</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate forcing|paleoclimatic modeling</Term>
    <Detailed_Variable>age,null,null,calendar year,null,climate forcing|paleoclimatic modeling,null,null,N,years from start of model simulation</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate forcing|paleoclimatic modeling</Term>
    <Detailed_Variable>carbon dioxide,null,null,parts per million,null,climate forcing|paleoclimatic modeling,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate forcing</Term>
    <Variable_Level_1>carbon dioxide</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>carbon cycle</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>56000000 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>55800000 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>Zeebe, R.E. 2012. 
LOSCAR: Long-term Ocean-atmosphere-Sediment CArbon cycle 
Reservoir Model v2.0.4. 
Geosci. Model Dev., 5, 149-166 
www.geosci-model-dev.net/5/149/2012/
doi:10.5194/gmd-5-149-2012</Reference>
  <Summary>
    <Abstract>The LOSCAR model is designed to efficiently compute the 
partitioning of carbon between ocean, atmosphere, and sediments 
on time scales ranging from centuries to millions of years. 
While a variety of computationally inexpensive carbon cycle 
models are already available, many are missing a critical 
sediment component, which is indispensable for long-term 
integrations. One of LOSCAR&apos;s strengths is the coupling 
of ocean-atmosphere routines to a computationally efficient 
sediment module. This allows, for instance, adequate computation 
of CaCO3 dissolution, calcite compensation, and long-term carbon 
cycle fluxes, including weathering of carbonate and silicate rocks. 
The ocean component includes various biogeochemical tracers 
such as total carbon, alkalinity, phosphate, oxygen, and stable 
carbon isotopes. LOSCAR&apos;s configuration of ocean geometry 
is flexible and allows for easy switching between modern 
and paleo-versions. We have previously published applications 
of the model tackling future projections of ocean chemistry 
and weathering, pCO2 sensitivity to carbon cycle perturbations 
throughout the Cenozoic, and carbon/calcium cycling during 
the Paleocene-Eocene Thermal Maximum. The focus of the present 
contribution is the detailed description of the model including 
numerical architecture, processes and parameterizations, tuning, 
and examples of input and output. Typical CPU integration times 
of LOSCAR are of order seconds for several thousand model years 
on current standard desktop machines. The LOSCAR source code 
in C can be obtained from the author by sending a request 
to loscar.model@gmail.com.

 
          STUDY NOTES: pCO2 output for the Palaeocene-Eocene Thermal Maximum from LOSCAR 
model (Long-term Ocean-atmosphere-Sediment CArbon cycle Reservoir Model)
Model run is for 200,000 y after Paleocene-Eocene boundary (~56 Ma)</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/climate_forcing/trace_gases/loscar-petm-co2.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/climate_forcing/trace_gases/loscar-petm-co2.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>
