{"xmlId":"17631","NOAAStudyId":"19802","studyName":"Eastern Labrador Sea Stable Isotope, Trace Metal and SST Data over the last 1250 Years","doi":"https://doi.org/10.25921/vb53-5v61","uuid":"999a65b6-9d88-4924-9161-c9646ff17f22","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":"PALEOCEANOGRAPHY","investigators":"Moffa-Sánchez, P.; Hall, I.R.; Barker, S.; Thornalley, D.J.R.; Yashayaev, I.M.","investigatorDetails":[{"firstName":"Paola","lastName":"Moffa-Sánchez","initials":"P.","orcId":"0000-0003-1857-8954"},{"firstName":"Ian","lastName":"Hall","initials":"I.R.","orcId":"0000-0001-6960-1419"},{"firstName":"Stephen","lastName":"Barker","initials":"S.","orcId":"0000-0001-7870-6431"},{"firstName":"David","lastName":"Thornalley","initials":"D.J.R.","orcId":"0000-0001-5885-5499"},{"firstName":"Igor","lastName":"Yashayaev","initials":"I.M.","orcId":null}],"version":"1.0","funding":[{"fundingAgency":"UK Natural Environment Research Council (NERC)","fundingGrant":null},{"fundingAgency":"Climate Change Consortium for Wales (C3W)","fundingGrant":null}],"studyNotes":"Provided Keywords: Last millennium, Labrador Sea","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/19802","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-19802.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-19802.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":["Sea Surface Temperature Reconstruction","Other Hydroclimate Reconstruction"],"reconstruction":"Y","contributionDate":"2016-02-22","entryId":"noaa-ocean-19802","earliestYearBP":1186,"mostRecentYearBP":35,"earliestYearCE":764,"mostRecentYearCE":1915,"publication":[{"author":{"name":"Moffa-Sánchez, P., I.R. Hall, S. Barker, D.J.R. Thornalley, and I. Yashayaev"},"pubYear":2014,"title":"Surface changes in the eastern Labrador Sea around the onset of the Little Ice Age","journal":"Paleoceanography","volume":"29","edition":null,"issue":null,"pages":"160-175","reportNumber":null,"citation":"Moffa-Sánchez, P., I.R. Hall, S. Barker, D.J.R. Thornalley, and I. Yashayaev. 2014. Surface changes in the eastern Labrador Sea around the onset of the Little Ice Age. Paleoceanography, 29, 160-175. doi: 10.1002/2013PA002523","type":"publication","identifier":{"type":"doi","id":"10.1002/2013PA002523","url":"http://dx.doi.org/10.1002/2013PA002523"},"abstract":"Despite the relative climate stability of the present interglacial, it has been punctuated by several centennial-scale climatic oscillations; the latest of which are often colloquially referred to as the Medieval Climatic Anomaly (MCA) and the Little Ice Age (LIA). The most favored explanation for the cause of these anomalies is that they were triggered by variability in solar irradiance and/or volcanic activity and amplified by ocean-atmosphere-sea ice feedbacks. As such, changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC) are widely believed to have been involved in the amplification of such climatic oscillations. The Labrador Sea is a key area of deep water formation. The waters produced here contribute approximately one third of the volume transport of the deep limb of the AMOC and drive changes in the North Atlantic surface hydrography and subpolar gyre circulation. In this study, we present multiproxy reconstructions from a high-resolution marine sediment core located south of Greenland that suggest an increase in the influence of polar waters reaching the Labrador Sea close to MCA-LIA transition. Changes in freshwater forcing may have reduced the formation of Labrador Sea Water and contributed toward the onset of the LIA cooling.","pubRank":"1"}],"site":[{"NOAASiteId":"56724","siteName":"RAPiD-35-25B","siteCode":null,"mappable":"Y","locationName":"Ocean>Atlantic Ocean>North Atlantic Ocean","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["57.507833","-48.723333"]},"properties":{"southernmostLatitude":"57.507833","northernmostLatitude":"57.507833","westernmostLongitude":"-48.723333","easternmostLongitude":"-48.723333","minElevationMeters":"-3486","maxElevationMeters":"-3486"}},"paleoData":[{"dataTableName":"RAPiD-35-25B POC 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