<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-tree-1003983</Entry_ID>
  <Entry_Title>NI LIBI Composite 1 Tree ring width, PAGES Australasia 2k Version</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Xiong, L.; Palmer, J.G.</Dataset_Creator>
    <Dataset_Title>NI LIBI Composite 1 Tree ring width, 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>10.25921/qzc1-wy05</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/1003983</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>L.</First_Name>
    <Last_Name>Xiong</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.G.</First_Name>
    <Last_Name>Palmer</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>tree-ring</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>1526 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1992 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>424 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-42 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>-39.5</Southernmost_Latitude>
    <Northernmost_Latitude>-39.5</Northernmost_Latitude>
    <Westernmost_Longitude>175.5</Westernmost_Longitude>
    <Easternmost_Longitude>175.5</Easternmost_Longitude>
    <Minimum_Altitude>1100</Minimum_Altitude>
    <Maximum_Altitude>1100</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>Australia/New Zealand</Location_Type>
    <Location_Subregion1>New Zealand</Location_Subregion1>
    <Detailed_Location>NI LIBI Composite 1&gt;LATITUDE -39.5&gt;LONGITUDE 175.5</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>Xiong, L.; Palmer, J</Author>
    <Publication_Date>2000</Publication_Date>
    <Title>Reconstruction of New Zealand Temperature Back to AD 1720 Using Libocedrus Bidwillii Tree rings</Title>
    <Volume>45</Volume>
    <Pages>339-359</Pages>
    <DOI>10.1029/2010pa002050</DOI>
  </Reference>
  <Reference>Neukom, R. and J. Gergis. 2012.
 Southern Hemisphere high-resolution palaeoclimate records 
of the last 2000 years. 
The Holocene, 22(5), 501-524.  
DOI: 10.1177/0959683611427335</Reference>
  <Summary>
    <Abstract>This study presents a comprehensive assessment of high-resolution 
Southern Hemisphere (SH) paleoarchives covering the last 2000 years. 
We identified 174 monthly to annually resolved climate proxy 
(tree ring, coral, ice core, documentary, speleothem and sedimentary) 
records from the Hemisphere. We assess the interannual and decadal 
sensitivity of each proxy record to large-scale circulation indices 
from the Pacific, Indian and Southern Ocean regions over the twentieth 
century. We then analyse the potential of this newly expanded 
palaeoclimate network to collectively represent predictands 
(sea surface temperature, sea level pressure, surface air temperature 
and precipitation) commonly used in climate reconstructions. 
The key dynamical centres-of-action of the equatorial Indo-Pacific 
are well captured by the palaeoclimate network, indicating that there 
is considerable reconstruction potential in this region, particularly 
in the post AD 1600 period when a number of long coral records are 
available. Current spatiotemporal gaps in data coverage and regions 
where significant potential for future proxy collection exists 
are discussed. We then highlight the need for new and extended records 
from key dynamical regions of the Southern Hemisphere. Although 
large-scale climate field reconstructions for the SH are in their 
infancy, we report that excellent progress in the development of 
regional proxies now makes plausible estimates of continental- 
to hemispheric-scale climate variations possible.
 
          STUDY NOTES: Uploaded by R. Neukom, data obtained from NOAA Paleo DB.
	 These are no raw data but processed and truncated chronologies, representing a composite of two or more individual sites. Details see (Neukom and Gergis 2011, The Holocene, DOI: 10.1177/0959683611427335). For the raws contact the authors or/and check ITRDB.</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/NI_LIBI_1.txt</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www.ncdc.noaa.gov/paleo/treering.html</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>
