{"xmlId":"20321","NOAAStudyId":"22278","studyName":"Lake Savine, French Mediterranean Alps 6,000 Year Flood Layer Data","doi":"https://doi.org/10.25921/7dck-5n37","uuid":"4db8024d-390b-4d75-b3f8-3c44ace24e74","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":"PALEOLIMNOLOGY","investigators":"Sabatier, P.; Wilhelm, B.; Ficetola, G.F.; Moiroux, F.; Poulenard, J.; Develle, A.-L.; Bichet, A.; Chen, W.; Pignol, C.; Reyss, J.-L.; Gielly, L.; Bajard, M.; Perrette, Y.; Malet, E.; Taberlet, P.; Arnaud, F.","investigatorDetails":[{"firstName":"Pierre","lastName":"Sabatier","initials":"P.","orcId":"0000-0002-9620-1514"},{"firstName":"Bruno","lastName":"Wilhelm","initials":"B.","orcId":"0000-0002-0555-1915"},{"firstName":"Gentile Francesco","lastName":"Ficetola","initials":"G.F.","orcId":"0000-0003-3414-5155"},{"firstName":"Fanny","lastName":"Moiroux","initials":"F.","orcId":null},{"firstName":"Jérôme","lastName":"Poulenard","initials":"J.","orcId":"0000-0003-0810-0308"},{"firstName":"Anne-Lise","lastName":"Develle","initials":"A.-L.","orcId":null},{"firstName":"Adéline","lastName":"Bichet","initials":"A.","orcId":"0000-0003-1409-1620"},{"firstName":"Wentao","lastName":"Chen","initials":"W.","orcId":null},{"firstName":"Cécile","lastName":"Pignol","initials":"C.","orcId":null},{"firstName":"Jean-Louis","lastName":"Reyss","initials":"J.-L.","orcId":null},{"firstName":"Ludovic","lastName":"Gielly","initials":"L.","orcId":null},{"firstName":"Manon","lastName":"Bajard","initials":"M.","orcId":null},{"firstName":"Yves","lastName":"Perrette","initials":"Y.","orcId":null},{"firstName":"Emmanuel","lastName":"Malet","initials":"E.","orcId":null},{"firstName":"Pierre","lastName":"Taberlet","initials":"P.","orcId":null},{"firstName":"Fabien","lastName":"Arnaud","initials":"F.","orcId":"0000-0002-8706-9902"}],"version":"1.0","funding":[{"fundingAgency":"French National Centre for Scientific Research (CNRS)","fundingGrant":"Hannibal Project"}],"studyNotes":"Sediment flood layer frequency and intensity data from Lake Savine, western Mediterranean Alps, for the past 6,000 years","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/22278","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-lake-22278.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-lake-22278.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/lake","studyCode":null,"scienceKeywords":["hydrology"],"reconstruction":"N","contributionDate":"2017-07-05","entryId":"noaa-lake-22278","earliestYearBP":5630,"mostRecentYearBP":-64,"earliestYearCE":-3680,"mostRecentYearCE":2014,"publication":[{"author":{"name":"Pierre Sabatier, Bruno Wilhelm, Gentile Francesco Ficetola, Fanny Moiroux, Jérôme Poulenard, Anne-Lise Develle, Adeline Bichet, Wentao Chen, Cécile Pignol, Jean-Louis Reyss, Ludovic Gielly, Manon Bajard, Yves Perrette, Emmanuel Malet, Pierre Taberlet, Fabien  Arnaud"},"pubYear":2017,"title":" 6-kyr record of flood frequency and intensity in the western Mediterranean Alps - Interplay of solar and temperature forcing","journal":"Quaternary Science Reviews","volume":"170","edition":null,"issue":null,"pages":"121-135","reportNumber":null,"citation":"Pierre Sabatier, Bruno Wilhelm, Gentile Francesco Ficetola, Fanny Moiroux, Jérôme Poulenard, Anne-Lise Develle, Adeline Bichet, Wentao Chen, Cécile Pignol, Jean-Louis Reyss, Ludovic Gielly, Manon Bajard, Yves Perrette, Emmanuel Malet, Pierre Taberlet, Fabien  Arnaud. 2017.  6-kyr record of flood frequency and intensity in the western Mediterranean Alps - Interplay of solar and temperature forcing. Quaternary Science Reviews, 170, 121-135. doi: 10.1016/j.quascirev.2017.06.019","type":"publication","identifier":{"type":"doi","id":"10.1016/j.quascirev.2017.06.019","url":"http://dx.doi.org/10.1016/j.quascirev.2017.06.019"},"abstract":"The high-resolution sedimentological and geochemical analysis of a sediment sequence from Lake Savine (Western Mediterranean Alps, France) led to the identification of 220 event layers for the last 6000 years. 200 were triggered by flood events and 20 by underwater mass movements possibly related to earthquakes that occurred in 5 clusters of increase seismicity. Because human activity could influence the flood chronicle, the presence of pastures was reconstructed through ancient DNA, which suggested that the flood chronicle was mainly driven by hydroclimate variability. Weather reanalysis of historical floods allow to identify that mesoscale precipitation events called \"East Return\" events were the main triggers of floods recorded in Lake Savine. The first part of this palaeoflood record (6-4 kyr BP) was characterized by increases in flood frequency and intensity in phase with Northern Alpine palaeoflood records. By contrast, the second part of the record (i.e., since 4 kyr BP) was phased with Southern Alpine palaeoflood records. These results suggest a palaeohydrological transition at approximately 4 kyr BP, as has been previously described for the Mediterranean region. This may have resulted in a change of flood-prone hydro-meteorological processes, i.e., in the balance between occurrence and intensity of local convective climatic phenomena and their influence on Mediterranean mesoscale precipitation events in this part of the Alps. At a centennial timescale, increases in flood frequency and intensity corresponded to periods of solar minima, affecting climate through atmospheric changes in the Euro-Atlantic sector.","pubRank":"1"}],"site":[{"NOAASiteId":"57277","siteName":"Lake Savine","siteCode":null,"mappable":"Y","locationName":"Continent>Europe>Western Europe>France","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["45.175","6.9137"]},"properties":{"southernmostLatitude":"45.175","northernmostLatitude":"45.175","westernmostLongitude":"6.9137","easternmostLongitude":"6.9137","minElevationMeters":"2447","maxElevationMeters":"2447"}},"paleoData":[{"dataTableName":"SAV14flood","NOAADataTableId":"33400","earliestYear":5630,"mostRecentYear":-64,"timeUnit":"cal yr BP","earliestYearBP":5630,"mostRecentYearBP":-64,"earliestYearCE":-3680,"mostRecentYearCE":2014,"coreLengthMeters":null,"dataTableNotes":null,"species":[],"dataFile":[{"fileUrl":"https://www.ncei.noaa.gov/pub/data/paleo/paleolimnology/europe/france/savine2017flood.txt","urlDescription":"NOAA Template File","linkText":"Lake Savine Flood Layer Data","variables":[{"cvDataType":"PALEOLIMNOLOGY","cvWhat":"age variable>age","cvMaterial":null,"cvError":null,"cvUnit":"time unit>age unit>calendar year before present","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOLIMNOLOGY","cvWhat":"formation property>event layer","cvMaterial":"geological material>bulk geological material>sediment","cvError":null,"cvUnit":"length unit>millimeter","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"underwater mass movement thickness","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOLIMNOLOGY","cvWhat":"formation property>event layer","cvMaterial":"geological material>bulk geological material>sediment","cvError":null,"cvUnit":"dimensionless","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"1=Mass Movement occurance 0=no Mass Movement","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOLIMNOLOGY","cvWhat":"formation property>event layer","cvMaterial":"geological material>bulk geological material>sediment","cvError":null,"cvUnit":"length unit>millimeter","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"flood layer thickness","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOLIMNOLOGY","cvWhat":"formation property>event layer","cvMaterial":"geological material>bulk geological material>sediment","cvError":null,"cvUnit":"dimensionless","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"1=flood occurance 0=no flood","cvFormat":"Numeric","cvShortName":null}],"NOAAKeywords":["earth science>paleoclimate>paleolimnology>physical properties"]}]}]}],"reference":{"pastThesaurusSkos":"https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf","pastThesaurusExplorer":"https://www.ncei.noaa.gov/access/paleo-search/cvterms","gcmdKeywordThesaurus":"https://earthdata.nasa.gov/earth-observation-data/find-data/idn/gcmd-keywords"},"dataLicenseDescription":null,"dataLicenseUrl":null}