NOAA/WDS Paleoclimatology - Upper Snake River 415 Year Streamflow Reconstructions
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title: NOAA/WDS Paleoclimatology - Upper Snake River 415 Year Streamflow Reconstructions
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Anchor: DOI doi:10.25921/nvkf-xr37
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abstract: This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Climate Reconstruction. The data include parameters of climate reconstructions|tree ring with a geographic location of Idaho, United States Of America. The time period coverage is from 359 to -58 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
purpose: Records of past temperature, precipitation, and other climate variables derived from paleoclimate proxies. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations.
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keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Paleoclimate Reconstructions
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keyword: earth science > paleoclimate > climate reconstructions|tree ring
keyword: earth science > paleoclimate > climate reconstructions|tree ring
keyword: earth science > paleoclimate > instrumental
keyword: earth science > paleoclimate > instrumental
keyword: earth science > paleoclimate > instrumental
keyword: earth science > paleoclimate > climate reconstructions|tree ring
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keyword: earth science > paleoclimate > reconstructions > streamflow
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keyword: Streamflow Reconstruction
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keyword: Continent > North America > United States Of America > Idaho > Palisades Dam > LATITUDE 43.3327 > LONGITUDE -111.2025
keyword: Continent > North America > United States Of America > Wyoming > Jackson Lake Dam > LATITUDE 43.8575 > LONGITUDE -110.59
keyword: Continent > North America > United States Of America > Idaho > Heise > LATITUDE 43.6419 > LONGITUDE -111.6844
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otherConstraints: Cite as: Wise, E.K. (2010-12-07): NOAA/WDS Paleoclimatology - Upper Snake River 415 Year Streamflow Reconstructions. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/nvkf-xr37. Accessed [date].
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otherConstraints: Distribution liability: NOAA and NCEI make no warranty, expressed or implied, regarding these data, nor does the fact of distribution constitute such a warranty. NOAA and NCEI cannot assume liability for any damages caused by any errors or omissions in these data. If appropriate, NCEI can only certify that the data it distributes are an authentic copy of the records that were accepted for inclusion in the NCEI archives.
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otherConstraints: 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.
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title: Tree ring record of streamflow and drought in the upper Snake River
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date: 2010
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individualName: Wise, E.K.
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description: Wise, E.K., 2010: Tree ring record of streamflow and drought in the upper Snake River. Water Resources Research, 46, , 10.1029/2010WR009282
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description: Date Range: 1591 CE to 2008 CE; Date Range: 359 cal yr BP to -58 cal yr BP;
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westBoundLongitude: -111.6844
eastBoundLongitude: -110.59
southBoundLatitude: 43.3327
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beginPosition: 1591
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supplementalInformation: 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: 43.8575N,-110.59W, 2065M (2) south fork of the Snake River at Palisades Dam, ID: 43.3327N, -111.2025W, 1708M (3) Snake River near Heise, ID: 43.6419N, -111.6844W, 1525M 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 SUPPLIED BY ORIGINATOR: 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'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.
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