<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-coral-1003975</Entry_ID>
  <Entry_Title>Havannah Coral Luminescence rainfall reconstruction, PAGES Australasia 2k Version</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Lough, J.M.</Dataset_Creator>
    <Dataset_Title>Havannah Coral Luminescence rainfall reconstruction, PAGES Australasia 2k Version</Dataset_Title>
    <Dataset_Release_Date>2013-02-28</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/1003975</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.M.</First_Name>
    <Last_Name>Lough</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|corals and sclerosponges</Term>
    <Detailed_Variable>precipitation,luminescence,null,millimeter,Oct-Mar,climate reconstructions|corals and sclerosponges,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|corals and sclerosponges</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|corals and sclerosponges,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>corals and sclerosponges</Term>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>PAGES 2k Network</Keyword>
  <Keyword>PAGES Australasia 2k</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1639 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1981 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>311 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-31 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-18</Southernmost_Latitude>
    <Northernmost_Latitude>-18</Northernmost_Latitude>
    <Westernmost_Longitude>147</Westernmost_Longitude>
    <Easternmost_Longitude>147</Easternmost_Longitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Ocean</Location_Category>
    <Location_Type>Pacific Ocean</Location_Type>
    <Detailed_Location>Havannah&gt;LATITUDE -18&gt;LONGITUDE 147</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>Lough, J.M.</Author>
    <Publication_Date>2011</Publication_Date>
    <Title>Great Barrier Reef coral luminescence reveals rainfall variability over northeastern Australia since the 17th century</Title>
    <Series>Paleoceanography</Series>
    <Volume>26</Volume>
    <Report_Number>PA2201</Report_Number>
    <DOI>10.1029/2010PA002050</DOI>
  </Reference>
  <Summary>
    <Abstract>Northeast tropical Queensland rainfall is concentrated in the summer 
half year and characterised by high interannual variability, partly 
related to El Niño-Southern Oscillation (ENSO) events. This results 
in highly variable river flows affecting near shore coral reefs of 
the Great Barrier Reef, Australia. Freshwater flood events are 
recorded in long-lived, annually-banded massive coral skeletons 
as luminescent lines.  Quantitative measurements of luminescence 
intensity were made for 20 Porites coral cores from near shore reef 
sites between 11°-23°S. Seventeen of the coral luminescence series 
were significantly correlated with an instrumental record of NE 
Queensland summer rainfall and used to develop seven significantly 
calibrated and verified rainfall reconstructions based on between 
17 (starting 1891) and one (starting 1639) coral series. The longest 
reconstruction, based on more than one coral, provides insights into 
NE Queensland rainfall variability from the late 17th century. 
Comparisons with various independent climate proxies are equivocal - 
the magnitude and significance of relationships with, for example, 
a proxy ENSO index vary through time. An extended drier period 
reconstructed from ~1760s to 1850s is associated with lower 
interannual rainfall variability. Since the late 19th century 
average rainfall and its variability have significantly increased 
with wet and dry extremes becoming more frequent than in earlier 
centuries. This suggests that a warming global climate maybe 
associated with more variable tropical Queensland rainfall. 
 
          STUDY NOTES: Uploaded by R. Neukom, data obtained from NOAA Paleo DB.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/reconstructions/pages2k/australasia2k/Havannah.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/coral/west_pacific/great_barrier/queensland-rainfall2011.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>
