<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-recon-16460</Entry_ID>
  <Entry_Title>White River, Arkansas 281 Year Flow Reconstruction</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Cleaveland, M.K.; Stahle, D.W.</Dataset_Creator>
    <Dataset_Title>White River, Arkansas 281 Year Flow Reconstruction</Dataset_Title>
    <Dataset_Release_Date>1994-07-01</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/16460</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>M.K.</First_Name>
    <Last_Name>Cleaveland</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.W.</First_Name>
    <Last_Name>Stahle</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|tree ring</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|tree ring,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|tree ring</Term>
    <Detailed_Variable>streamflow,null,null,cubic kilometer,Jan-Dec,climate reconstructions|tree ring,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>reconstructions</Term>
    <Variable_Level_1>streamflow</Variable_Level_1>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Streamflow Reconstruction</Keyword>
  <Keyword>hydrology</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1700 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>1980 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>250 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-30 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>34.686</Southernmost_Latitude>
    <Northernmost_Latitude>34.686</Northernmost_Latitude>
    <Westernmost_Longitude>-91.3154</Westernmost_Longitude>
    <Easternmost_Longitude>-91.3154</Easternmost_Longitude>
    <Minimum_Altitude>53</Minimum_Altitude>
    <Maximum_Altitude>53</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Arkansas</Location_Subregion2>
    <Detailed_Location>Clarendon&gt;LATITUDE 34.686&gt;LONGITUDE -91.3154</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>Malcolm K. Cleaveland and David W. Stahle</Author>
    <Publication_Date>1989</Publication_Date>
    <Title>Tree ring analysis of surplus and deficit runoff in the White River, Arkansas</Title>
    <Series>Water Resources Research</Series>
    <Volume>25</Volume>
    <Issue>6</Issue>
    <Pages>1391-1401</Pages>
    <DOI>10.1029/WR025i006p01391</DOI>
    <Online_Resource>http://onlinelibrary.wiley.com/doi/10.1029/WR025i006p01391/abstract</Online_Resource>
  </Reference>
  <Summary>
    <Abstract>A 281-year reconstruction of White River calendar year runoff at Clarendon, Arkansas, was developed from a regional average of nine tree ring chronologies in Oklahoma, Missouri, and Arkansas (including six post oak and three bald cypress chronologies). Inhomogeneity of the gaged runoff series prior to 1930 was detected with two independent double mass analyses, comparing the gaged data with Arkansas state average annual precipitation and the regional tree ring chronology average. The homogeneous runoff data from 1930 to 1980 were calibrated with the average tree ring data using regression. The variance of the reconstruction increases significantly during the twentieth century and may reflect climatic change and/or anthropogenic disturbances in the watershed. Years of surplus and deficit runoff are nonrandomly distributed in both the gaged and reconstructed series. This nonrandomness appears to be caused primarily by interannual persistence of runoff extremes, which may provide a basis for some improvement of probabilistic forecasts of annual runoff for the White River. 
          STUDY NOTES: Reconstructed Annual (Calendar Yr) Runoff of the White River at Clarendon, Arkansas (Cubic Km/Yr). ID=RCLROM3X</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/treering/reconstructions/southusa/whiteriv.rec</URL>
    <Description>Data File; White River 281 Year Flow Reconstruction </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>2019-05-30</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2019-05-29</Last_DIF_Revision_Date>
</DIF>
