<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-pollen-19764</Entry_ID>
  <Entry_Title>Falkland Islands 2600 Year Pollen and Charcoal Data</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Turney, C.S.M.; Jones, R.T.; Fogwill, C.; Hatton, J.; Williams, A.N.; Hogg, A.; Thomas, Z.A.; Mooney, S.; Reimer, R.W.</Dataset_Creator>
    <Dataset_Title>Falkland Islands 2600 Year Pollen and Charcoal Data</Dataset_Title>
    <Dataset_Release_Date>2016-02-02</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/19764</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.S.M.</First_Name>
    <Last_Name>Turney</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.T.</First_Name>
    <Last_Name>Jones</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>C.</First_Name>
    <Last_Name>Fogwill</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.</First_Name>
    <Last_Name>Hatton</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.N.</First_Name>
    <Last_Name>Williams</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>A.</First_Name>
    <Last_Name>Hogg</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>Z.A.</First_Name>
    <Last_Name>Thomas</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>S.</First_Name>
    <Last_Name>Mooney</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>R.W.</First_Name>
    <Last_Name>Reimer</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>pollen</Term>
    <Variable_Level_1>population abundance</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Antarctic Oscillation (AAO)</Keyword>
  <Keyword>Southern Annular Mode (SAM)</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>2623 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-60 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-51.691</Southernmost_Latitude>
    <Northernmost_Latitude>-51.691</Northernmost_Latitude>
    <Westernmost_Longitude>-57.785</Westernmost_Longitude>
    <Easternmost_Longitude>-57.785</Easternmost_Longitude>
    <Minimum_Altitude>30</Minimum_Altitude>
    <Maximum_Altitude>30</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Atlantic Ocean</Location_Type>
    <Location_Subregion1>South Atlantic Ocean</Location_Subregion1>
    <Location_Subregion2>Falkland Islands</Location_Subregion2>
    <Detailed_Location>Canopus Hill&gt;LATITUDE -51.691&gt;LONGITUDE -57.785</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>
    <Author>Turney, C.S.M., Jones, R.T., Fogwill, C., Hatton, J., Williams, A.N., Hogg, A., Thomas, Z.A., Palmer, J., Mooney, S., Reimer, R.W.</Author>
    <Publication_Date>2016</Publication_Date>
    <Title>A 250-year periodicity in Southern Hemisphere westerly winds over the last 2600 years</Title>
    <Series>Climate of the Past</Series>
    <Volume>12</Volume>
    <Issue>2</Issue>
    <Pages>1-12</Pages>
    <DOI>10.5194/cp-12-1-2016</DOI>
    <Online_Resource>http://www.clim-past.net/12/189/2016/</Online_Resource>
  </Reference>
  <Summary>
    <Abstract>Southern Hemisphere westerly airflow has a significant influence on the ocean-atmosphere system of the mid- to high latitudes with potentially global climate implications. Unfortunately, historic observations only extend back to the late 19th century, limiting our understanding of multi-decadal to centennial change. Here we present a highly resolved (30-year) record of past westerly wind strength from a Falkland Islands peat sequence spanning the last 2600 years. Situated within the core latitude of Southern Hemisphere westerly airflow (the so-called furious fifties), we identify highly variable changes in exotic pollen and charcoal derived from South America which can be used to inform on past westerly air strength. We find a period of high charcoal content between 2000 and 1000 cal.years BP, associated with increased burning in Patagonia, most probably as a result of higher temperatures and stronger westerly airflow. Spectral analysis of the charcoal record identifies a pervasive ca. 250-year  periodicity that is coherent with radiocarbon production rates, suggesting that solar variability has a modulating influence on Southern Hemisphere westerly airflow. Our results have important implications for understanding global climate change through the late Holocene.  
          STUDY NOTES: Pollen and charcoal record from peat sequence spanning the last 2600 years, with exotic input from Patagonia.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/pollen/southamerica/falkland2016pollen.txt</URL>
    <Description>Data File; Falkland Islands Pollen and Charcoal Data </Description>
  </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>2019-07-03</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-07-03</Last_DIF_Revision_Date>
</DIF>
