{"xmlId":"80431","NOAAStudyId":"39277","studyName":"Touchan - Col de Saltu, Corsica - PINI - ITRDB FRA059","doi":"https://doi.org/10.25921/c998-ca53","uuid":"503b1d88-bd10-428d-afa0-e4721eb05c05","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":"Touchan, R.","investigatorDetails":[{"firstName":"Ramzi","lastName":"Touchan","initials":"R.","orcId":null}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/39277","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-tree-39277.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-tree-39277.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/tree-ring","studyCode":"FRA059","scienceKeywords":["Pinus nigra J.F. Arnold","Austrian pine","PINI","black pine"],"reconstruction":"N","contributionDate":"2024-04-05","entryId":"noaa-tree-39277","earliestYearBP":564,"mostRecentYearBP":-63,"earliestYearCE":1386,"mostRecentYearCE":2013,"publication":[{"author":{"name":"Touchan, Ramzi; Kevin J Anchukaitis; David M Meko; Dalila Kerchouche; Said Slimani; Rachid Ilmen; Fouad Hasnaoui; Frederic Guibal; Jesus Julio Camarero; Raúl Sánchez-Salguero; Alma Piermattei; Abdessadek Sesbou; Benjamin I Cook; Mohamed Sabir; Hayat Touchane"},"pubYear":2017,"title":"Climate controls on tree growth in the Western Mediterranean","journal":"The Holocene","volume":"27","edition":null,"issue":"10","pages":"1429-1442","reportNumber":null,"citation":"Touchan, Ramzi; Kevin J Anchukaitis; David M Meko; Dalila Kerchouche; Said Slimani; Rachid Ilmen; Fouad Hasnaoui; Frederic Guibal; Jesus Julio Camarero; Raúl Sánchez-Salguero; Alma Piermattei; Abdessadek Sesbou; Benjamin I Cook; Mohamed Sabir; Hayat Touchane. 2017. Climate controls on tree growth in the Western Mediterranean. The Holocene, 27(10), 1429-1442. doi: 10.1177/0959683617693901","type":"publication","identifier":{"type":"doi","id":"10.1177/0959683617693901","url":"http://dx.doi.org/10.1177/0959683617693901"},"abstract":"The first large-scale network of tree-ring chronologies from the western Mediterranean (WM; 32°N43°N, 10°W17°E) is described and analyzed to identify the seasonal climatic signal in indices of annual ring width. Correlation and rotated empirical orthogonal function analyses are applied to 85 tree-ring series and corresponding gridded climate data to assess the climate signal embedded in the network. Chronologies range in length from 80 to 1129 years. Monthly correlations and partial correlations show overall positive associations for Pinus halepensis (PIHA) and Cedrus atlantica (CDAT) with winter (DecemberFebruary) and spring (MarchMay) precipitation across this network. In both seasons, the precipitation correlation with PIHA is stronger, while CDAT chronologies tend to be longer. A combination of positive correlations between growth and wintersummer precipitation and negative partial correlations with growing season temperatures suggests that chronologies in at least part of the network reflect soil moisture and the integrated effects of precipitation and evapotranspiration signal. The range of climate response observed across this network reflects a combination of both species and geographic influences. Western Moroccan chronologies have the strongest association with the North Atlantic Oscillation.","pubRank":"1"}],"site":[{"NOAASiteId":"60234","siteName":"Col de Saltu, Corsica","siteCode":null,"mappable":"Y","locationName":"Continent>Europe>Western Europe>France","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["42.28","8.83"]},"properties":{"southernmostLatitude":"42.28","northernmostLatitude":"42.28","westernmostLongitude":"8.83","easternmostLongitude":"8.83","minElevationMeters":"1433","maxElevationMeters":"1433"}},"paleoData":[{"dataTableName":"FRA059","NOAADataTableId":"52075","earliestYear":1386,"mostRecentYear":2013,"timeUnit":"CE","earliestYearBP":564,"mostRecentYearBP":-63,"earliestYearCE":1386,"mostRecentYearCE":2013,"coreLengthMeters":null,"dataTableNotes":null,"species":[{"speciesCode":"PINI","scientificName":"Pinus nigra J.F. 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