{"xmlId":"17834","NOAAStudyId":"19970","studyName":"Brown - Hoback Ridge - PSME - ITRDB WY055","doi":"https://doi.org/10.25921/6htb-kw64","uuid":"f4d39bed-1eef-4d94-8fc2-239f19bc8e4d","dataPublisher":"NOAA","contactInfo":{"type":"CONTACT INFORMATION","shortName":"DOC/NOAA/NESDIS/NCEI","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","address":"325 Broadway, E/NE31","city":"Boulder","state":"CO","postalCode":"80305-3328","country":"USA","dataCenterUrl":"https://www.ncei.noaa.gov/products/paleoclimatology","email":"paleo@noaa.gov","phone":"828-271-4800","fax":null,"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."},"dataType":"TREE RING","investigators":"Brown, P.; Wise, E.K.","investigatorDetails":[{"firstName":"Paul","lastName":"Brown","initials":"P.","orcId":null},{"firstName":"Erika","lastName":"Wise","initials":"E.K.","orcId":"0000-0002-1712-7476"}],"version":"1.0","funding":[],"studyNotes":"Collected by staff from the Teton Science School.  Dated and measured by Paul Brown.  Submitted by Erika Wise, with permission from Teton Science School.  Funded by: Teton Science School.  Utilized in Upper Snake River Flow reconstruction archived at NOAA/WDC Paleoclimatology: \r\nhttps://www.ncei.noaa.gov/pub/data/paleo/treering/reconstructions/northamerica/usa/idaho/snake-flow2010.txt \r\nhttps://www.ncei.noaa.gov/pub/data/paleo/treering/reconstructions/northamerica/usa/idaho/snake-flow2010.xls  NOAA Template Raw Measurements file added 2019-02-08.","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/19970","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-tree-19970.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-tree-19970.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/tree-ring","studyCode":"WY055","scienceKeywords":["Douglas-fir","PSME","Pseudotsuga menziesii (Mirb.) Franco"],"reconstruction":"N","contributionDate":"2016-01-19","entryId":"noaa-tree-19970","earliestYearBP":366,"mostRecentYearBP":-56,"earliestYearCE":1584,"mostRecentYearCE":2006,"publication":[{"author":{"name":"Wise, E.K."},"pubYear":2010,"title":"Tree ring record of streamflow and drought in the upper Snake River","journal":"Water Resources Research","volume":"46","edition":null,"issue":"11","pages":null,"reportNumber":"W11529","citation":"Wise, E.K. 2010. Tree ring record of streamflow and drought in the upper Snake River. Water Resources Research, 46(11), W11529. doi: 10.1029/2010WR009282","type":"publication","identifier":{"type":"doi","id":"10.1029/2010WR009282","url":"http://dx.doi.org/10.1029/2010WR009282"},"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'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.","pubRank":"1"}],"site":[{"NOAASiteId":"56776","siteName":"Hoback Ridge","siteCode":null,"mappable":"Y","locationName":"Continent>North America>United States Of America>Wyoming","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["43.3042","-110.6711"]},"properties":{"southernmostLatitude":"43.3042","northernmostLatitude":"43.3042","westernmostLongitude":"-110.6711","easternmostLongitude":"-110.6711","minElevationMeters":"1997","maxElevationMeters":"1997"}},"paleoData":[{"dataTableName":"WY055","NOAADataTableId":"30638","earliestYear":1584,"mostRecentYear":2006,"timeUnit":"CE","earliestYearBP":366,"mostRecentYearBP":-56,"earliestYearCE":1584,"mostRecentYearCE":2006,"coreLengthMeters":null,"dataTableNotes":null,"species":[{"speciesCode":"PSME","scientificName":"Pseudotsuga menziesii (Mirb.) 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