<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-9890</Entry_ID>
  <Entry_Title>Upper Snake River 415 Year Streamflow Reconstructions </Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Wise, E.K.</Dataset_Creator>
    <Dataset_Title>Upper Snake River 415 Year Streamflow Reconstructions </Dataset_Title>
    <Dataset_Release_Date>2010-12-07</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/9890</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>E.K.</First_Name>
    <Last_Name>Wise</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,acre foot,Oct-Sep,climate reconstructions|tree ring,null,null,N,Jackson Lake at Dam on Snake River near Moran WY</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>instrumental</Term>
    <Detailed_Variable>streamflow,null,null,acre foot,Oct-Sep,instrumental,null,null,N,Snake River near Heise ID</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|tree ring</Term>
    <Detailed_Variable>streamflow,null,null,acre foot,Oct-Sep,climate reconstructions|tree ring,null,null,N,south fork of the Snake River at Palisades Dam ID</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>instrumental</Term>
    <Detailed_Variable>streamflow,null,null,acre foot,Oct-Sep,instrumental,null,null,N,Jackson Lake at Dam on Snake River near Moran WY</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|tree ring</Term>
    <Detailed_Variable>streamflow,null,null,acre foot,Oct-Sep,climate reconstructions|tree ring,null,null,N,Snake River near Heise ID</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>instrumental</Term>
    <Detailed_Variable>streamflow,null,null,acre foot,Oct-Sep,instrumental,null,null,N,south fork of the Snake River at Palisades Dam ID</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>drought</Keyword>
  <Keyword>hydrology</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>1591 AD</Paleo_Start_Date>
    <Paleo_Stop_Date>2005 AD</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>359 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>-55 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>43.3327</Southernmost_Latitude>
    <Northernmost_Latitude>43.8575</Northernmost_Latitude>
    <Westernmost_Longitude>-111.6844</Westernmost_Longitude>
    <Easternmost_Longitude>-110.59</Easternmost_Longitude>
    <Minimum_Altitude>1525</Minimum_Altitude>
    <Maximum_Altitude>2065</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>Idaho</Location_Subregion2>
    <Detailed_Location>Palisades Dam&gt;LATITUDE 43.3327&gt;LONGITUDE -111.2025</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Idaho</Location_Subregion2>
    <Detailed_Location>Heise&gt;LATITUDE 43.6419&gt;LONGITUDE -111.6844</Detailed_Location>
  </Location>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Wyoming</Location_Subregion2>
    <Detailed_Location>Jackson Lake Dam&gt;LATITUDE 43.8575&gt;LONGITUDE -110.59</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>Wise, E.K. 2010. 
Tree ring record of streamflow and drought in the upper Snake River. 
Water Resources Research, Vol. 46 (W11529). 
doi:10.1029/2010WR009282. 
</Reference>
  <Summary>
    <Abstract>Tree ring samples collected near the Snake River headwaters 
were augmented with preexisting tree ring chronologies to create 
a 415 year reconstruction of upper Snake River streamflow, 
extending the short instrumental record and providing the first 
description of multicentury water supply variability in this river. 
Results indicate that the region&apos;s early 21st century drought 
is severe even in the context of long-term climatic variability 
and that the instrumental record is representative of low-flow 
individual years. In terms of overall magnitude, droughts of the 
recent past are eclipsed by a sustained low-flow period lasting 
for over 30 years in the early to mid-1600s. A comparison of 
reconstructed Snake River flow with streamflow reconstructions 
of the Colorado, Sacramento, and Verde rivers suggests that 
changes in the predominance of zonal versus meridional atmospheric 
flow may have influenced drought patterns in the western 
United States through time. 
 
          STUDY NOTES: Wise 2010 tree-ring reconstruction of streamflow at three gages in 
the upper Snake River.  Reconstruction is of total annual (water year) 
flow in acre-feet.  The reconstructed gage records are for the 
following gages: 
(1) Jackson Lake at Dam on Snake River near Moran, WY 
(2) south fork of the Snake River at Palisades Dam, ID 
(3) Snake River near Heise, ID. 

Reconstruction is based on 3 tree-ring chronologies: 
FMT Douglas fir (S. Gray): 42.96°N, 109.77°W, 2300m, 1507-2006AD 
HRI Limber pine (Teton Science School): 43.30°N, 110.67°W, 2000m 1505-2006AD 
RDH Limber pine (E. Wise): 43.62°N, 110.44°W, 2300m, 1322-2006AD 

The RDH chronology is archived in the International Tree Ring Data Bank (ITRDB): 
http://www.ncdc.noaa.gov/paleo/treering.html 

Instrumental data was supplied by the U.S. Bureau of Reclamation 
(http://www.usbr.gov/pn/hydromet).  See Wise (2010) for 
more complete description of data and methods. 


</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/northamerica/usa/idaho/snake-flow2010.xls</URL>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/treering/reconstructions/northamerica/usa/idaho/snake-flow2010.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>
