{"NOAAStudyId":"25692","contactInfo":{"address":"325 Broadway, E/NE31","city":"Boulder","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.","country":"USA","dataCenterUrl":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data","email":"paleo@noaa.gov","fax":"303-497-6513","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","phone":"303-497-6280","postalCode":"80305-3328","shortName":"DOC/NOAA/NESDIS/NCEI","state":"CO","type":"CONTACT INFORMATION"},"contributionDate":"2018-11-21","dataPublisher":"NOAA","dataType":"TREE RING","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/tree-ring","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-tree-25692.xml","doi":"https://doi.org/10.25921/y4pb-3488","earliestYearBP":303,"earliestYearCE":1647,"entryId":"noaa-tree-25692","funding":[],"investigators":"Cerrato, R.; Baroni, C.","mostRecentYearBP":-66,"mostRecentYearCE":2016,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/25692","originalSource":null,"publication":[{"abstract":"Ongoing climate change strongly affects high-elevation environments in the European Alps, influencing the cryosphere and the biosphere and causing widespread retreat of glaciers and changes in biomes. Nevertheless, high-elevation areas often lack long meteorological series, and global datasets cannot represent local variations well. Thus, proxy data, such as tree rings, provide information on past climatic variations from these remote sites. Although maximum latewood density (MXD) chronologies provide better temperature information than those based on tree-ring width (TRW), MXD series from the European Alps are lacking. To derive high-quality temperature information for the Rhaetian Alps, Pinus cembra L. trees sampled at approximately 2000 m a.s.l. were used to build one MXD chronology spanning from 1647 to 2015. The MXD data were significantly and highly correlated with seasonal May-September mean temperatures. The MXD chronology showed a generally positive trend since the middle of the 19th century, interrupted by short phases of climatic deterioration in the beginning of the 20th century and in the 1970s, conforming with the temperature trends. Our results underline the potential for using Pinus cembra L. MXD to reconstruct mean temperature variations, especially during the onset and latter part of the growing season, providing additional information on parts of the growing season not inferred from TRW. Future studies on MXD for this species will increase the availability of temporal and spatial data, allowing detailed climate reconstructions.","author":{"name":"Riccardo Cerrato, Maria Cristina Salvatore, Björn E. Gunnarson, Hans W. Linderholm, Luca Carturan, Michele Brunetti, Fabrizio De Blasi, Carlo Baroni"},"citation":"Riccardo Cerrato, Maria Cristina Salvatore, Björn E. Gunnarson, Hans W. Linderholm, Luca Carturan, Michele Brunetti, Fabrizio De Blasi, Carlo Baroni. 2019. A Pinus cembra L. tree-ring record for late spring to late summer temperature in the Rhaetian Alps, Italy. Dendrochronologia, 53, 2-31. doi: 10.1016/j.dendro.2018.10.010","edition":null,"identifier":{"id":"10.1016/j.dendro.2018.10.010","type":"doi","url":"http://dx.doi.org/10.1016/j.dendro.2018.10.010"},"issue":null,"journal":"Dendrochronologia","pages":"2-31","pubRank":"1","pubYear":2019,"reportNumber":null,"title":"A Pinus cembra L. tree-ring record for late spring to late summer temperature in the Rhaetian Alps, Italy","type":"publication","volume":"53"}],"reconstruction":"N","scienceKeywords":["Swiss stone pine","PICE","Pinus cembra L.","Arolla pine"],"site":[{"NOAASiteId":"57758","geo":{"geoType":"Feature","geometry":{"coordinates":["46.4203","10.68525"],"type":"POINT"},"properties":{"easternmostLongitude":"10.68525","maxElevationMeters":"2250","minElevationMeters":"2250","northernmostLatitude":"46.4203","southernmostLatitude":"46.4203","westernmostLongitude":"10.68525"}},"locationName":"Continent>Europe>Southern Europe>Italy","mappable":"Y","paleoData":[{"NOAADataTableId":"37555","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>tree-ring>width>ring width"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/correlation-stats/ital051.txt","linkText":"ital051.txt","urlDescription":"Correlation Stats","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>tree-ring>width>ring width"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/ital051.rwl","linkText":"ital051.rwl","urlDescription":"Raw Measurements","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>tree-ring>width>earlywood width"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/ital051e.rwl","linkText":"ital051e.rwl","urlDescription":"Raw Measurements","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>tree-ring>width>latewood width"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/ital051l.rwl","linkText":"ital051l.rwl","urlDescription":"Raw Measurements","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>tree-ring>density>minimum density"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/ital051n.rwl","linkText":"ital051n.rwl","urlDescription":"Raw Measurements","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>tree-ring>density>maximum density"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/ital051x.rwl","linkText":"ital051x.rwl","urlDescription":"Raw Measurements","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>tree-ring>width>ring width"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/treering/measurements/europe/ital051n-noaa.rwl","linkText":"ital051n-noaa.rwl","urlDescription":"Raw Measurements - NOAA Template File","variables":[{"cvAdditionalInfo":"Tree ID: VLAM01; 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