{"xmlId":"1587","NOAAStudyId":"2588","studyName":"Interglacial North Atlantic Temperature and Salinity Data","doi":"https://doi.org/10.25921/hxcm-cv24","uuid":"a839af0c-1323-4f1d-bb98-0743ea600432","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":"Cortijo, E.; Lehman, S.J.; Keigwin, L.D.; Chapman, M.R.; Paillard, D.; Labeyrie, L.D.","investigatorDetails":[{"firstName":"Elsa","lastName":"Cortijo","initials":"E.","orcId":null},{"firstName":"Scott","lastName":"Lehman","initials":"S.J.","orcId":null},{"firstName":"Lloyd","lastName":"Keigwin","initials":"L.D.","orcId":null},{"firstName":"Mark","lastName":"Chapman","initials":"M.R.","orcId":null},{"firstName":"Didier","lastName":"Paillard","initials":"D.","orcId":"0000-0002-9995-2794"},{"firstName":"Laurent","lastName":"Labeyrie","initials":"L.D.","orcId":"0000-0002-1554-2449"}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/2588","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-2588.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-2588.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":null,"reconstruction":"Y","contributionDate":"1999-07-01","entryId":"noaa-ocean-2588","earliestYearBP":null,"mostRecentYearBP":null,"earliestYearCE":null,"mostRecentYearCE":null,"publication":[{"author":{"name":"Cortijo, E., S.J. Lehman, L.D. Keigwin, M.R. Chapman, D. Paillard, and L. Labeyrie"},"pubYear":1999,"title":"Changes in meridional temperature and salinity gradients in the North Atlantic Ocean (30-72N) during the last interglacial period","journal":"Paleoceanography","volume":"14","edition":null,"issue":"1","pages":"22-33","reportNumber":null,"citation":"Cortijo, E., S.J. Lehman, L.D. Keigwin, M.R. Chapman, D. Paillard, and L. Labeyrie. 1999. Changes in meridional temperature and salinity gradients in the North Atlantic Ocean (30-72N) during the last interglacial period. Paleoceanography, 14(1), 22-33. doi: 10.1029/1998PA900004","type":"publication","identifier":{"type":"doi","id":"10.1029/1998PA900004","url":"http://dx.doi.org/10.1029/1998PA900004"},"abstract":"Eight deep-sea sediment cores from the North Atlantic Ocean ranging from 31° to 72°N are studied to reconstruct the meridional gradients in surface hydrographic conditions during the interval of minimum ice volume within the last interglacial period. Using benthic foraminiferal ´18O measurements and estimates of Sea Surface Temperature (SST) and Sea Surface Salinity (SSS), we show that summer SSTs and SSSs decreased gradually during the interval of minimum ice volume at high-latitude sites (52°72°N) whereas they were stable or increased during the same time period at low-latitude sites (31°41°N). This increase in meridional gradients of SSTs and SSSs may have been due to changes in the latitudinal distribution of summer and annual-average insolation and associated oceanic and atmospheric feedbacks. These trends documented for the Eemian ice volume minimum period are similar to corresponding changes observed during the Holocene and may have had a similar origin.","pubRank":"1"}],"site":[{"NOAASiteId":"17905","siteName":"V27-60","siteCode":null,"mappable":"Y","locationName":"Ocean>Arctic Ocean","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["72.18","8.58"]},"properties":{"southernmostLatitude":"72.18","northernmostLatitude":"72.18","westernmostLongitude":"8.58","easternmostLongitude":"8.58","minElevationMeters":"-2525","maxElevationMeters":"-2525"}},"paleoData":[{"dataTableName":"V27-60C","NOAADataTableId":"4234","earliestYear":null,"mostRecentYear":null,"timeUnit":null,"earliestYearBP":null,"mostRecentYearBP":null,"earliestYearCE":null,"mostRecentYearCE":null,"coreLengthMeters":null,"dataTableNotes":"Benthic foraminifer d18O measurements used for the definition of the 5e plateau. 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