{"NOAAStudyId":"10890","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":"2011-04-22","dataPublisher":"NOAA","dataType":"PALEOCEANOGRAPHY","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/paleoceanography","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-10890.xml","doi":null,"earliestYearBP":1948,"earliestYearCE":2,"entryId":"noaa-ocean-10890","funding":[{"fundingAgency":"US National Science Foundation","fundingGrant":null}],"investigators":"Keigwin, L.D.; Pickart, R.S.","mostRecentYearBP":17,"mostRecentYearCE":1933,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/10890","originalSource":null,"publication":[{"abstract":"The strength and position of surface and deep currents \nin the slope water south of Newfoundland are thought \nto vary as a coupled system in relation to the dipole \nin atmospheric sea level pressure known as the North \nAtlantic oscillation (NAO). Paleoceanographic data \nfrom the Laurentian Fan, used as a proxy for sea surface \ntemperature, reveal that surface slope waters north of \nthe Gulf Stream experienced warming during the Little \nIce Age of the 16th to 19th centuries and support the \nnotion of an NAO-driven coupled system. The NAO may be \na useful model for millennial-scale ocean variability \nduring interglacial climate states. \n","author":null,"citation":"Keigwin, L.D. and R.S. Pickart. 1999. \nSlope Water Current over the Laurentian Fan on Interannual \nto Millennial Time Scales. \nScience, Vol. 286, no. 5439, pp. 520-523, 15 October 1999. \nDOI: 10.1126/science.286.5439.520 \n\n","edition":null,"identifier":{"id":"10.1126/science.286.5439.520","type":"doi","url":"http://dx.doi.org/10.1126/science.286.5439.520"},"issue":null,"journal":"Science","pages":null,"pubRank":"1","pubYear":1999,"reportNumber":null,"title":"Slope Water Current over the Laurentian Fan on Interannual  to Millennial Time Scales","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":["North Atlantic Oscillation"],"site":[{"NOAASiteId":"48000","geo":{"geoType":"Feature","geometry":{"coordinates":["43.0833","-55.8"],"type":"POINT"},"properties":{"easternmostLongitude":"-55.8","maxElevationMeters":"-3440","minElevationMeters":"-3440","northernmostLatitude":"43.0833","southernmostLatitude":"43.0833","westernmostLongitude":"-55.8"}},"locationName":"Ocean>Atlantic 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Data include \nN.pachy.s. and total planktonic foraminifera counts, \nplus carbonate content and sediment \"redness\" measurements.  \n","version":"1.0","xmlId":"9453"}