{"NOAAStudyId":"11171","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":"2011-05-11","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-11171.xml","doi":null,"earliestYearBP":959,"earliestYearCE":991,"entryId":"noaa-ocean-11171","funding":[{"fundingAgency":"Gary Comer Science and Education Foundation","fundingGrant":null},{"fundingAgency":"Norwegian Research Council (NCR)","fundingGrant":null}],"investigators":"Sejrup, H.P.; Lehman, S.J.; Haflidason, H.; Noone, D.; Muscheler, R.; Berstad, I.M.; Andrews, J.T.","mostRecentYearBP":-48,"mostRecentYearCE":1998,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/11171","originalSource":null,"publication":[{"abstract":"We report on a 1000 year long oxygen isotope record in sediments \r\nof the eastern Norwegian Sea which, we argue, represents the \r\ntemperature and transport of warm Atlantic waters entering the \r\nNordic Sea basin via the North Atlantic Drift and the large-scale \r\nMeridional Overturning Circulation. The single-sample resolution \r\nof the record is 2.5-10 years and age control is provided by 210Pb \r\nand 137Cs dating, identification of historic tephra, and a 14C \r\n\"wiggle-match\" dating method in which the surface reservoir 14C age \r\nin the past is constrained rather than assumed, thereby eliminating \r\na large source of chronological uncertainty. The oxygen isotope \r\nresults indicate decade- to century-scale temperature variations \r\nof 1-2°C in the shallow (~50 m deep) subsurface which we find to be \r\nstrongly correlated with various proxies of past solar activity. \r\nThe correlations are synchronous to within the timescale uncertainties \r\nof the ocean and solar proxy records, which vary among the records \r\nand in time with a range of about 5-30 years. The observed ocean \r\ntemperature response is larger than expected based on simple \r\nthermodynamic considerations, indicating that there is dynamical \r\nresponse of the high-latitude ocean to the Sun. Correlations of our \r\nresults with a gridded temperature reconstruction for Europe are \r\ngreater in central Europe than in coastal regions, suggesting that \r\nthe temperature and transport of warm Atlantic waters entering \r\nthe Nordic Basin and the pattern of temperature variability over \r\nEurope are both the proximate responses to a change in the \r\natmospheric circulation, consistent with a forced shift in the \r\nprimary modes of high-latitude atmospheric variability. ","author":null,"citation":"Sejrup, H.P., S.J. Lehman, H. Haflidason, D. Noone, R. Muscheler, \r\nI.M. Berstad, and J.T. Andrews. 2010. \r\nResponse of Norwegian Sea temperature to solar forcing since 1000 A.D. \r\nJournal of Geophysical Research, Vol. 115, C12034. \r\ndoi:10.1029/2010JC006264. ","edition":null,"identifier":{"id":"10.1029/2010JC006264","type":"doi","url":"http://dx.doi.org/10.1029/2010JC006264"},"issue":null,"journal":"Journal of Geophysical Research: Oceans","pages":null,"pubRank":"1","pubYear":2010,"reportNumber":null,"title":"Response of Norwegian Sea temperature to solar forcing since 1000 A.D. ","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":["Meridional Overturning Circulation (MOC)"],"site":[{"NOAASiteId":"48079","geo":{"geoType":"Feature","geometry":{"coordinates":["63.7622","5.2553"],"type":"POINT"},"properties":{"easternmostLongitude":"5.2553","maxElevationMeters":"-851","minElevationMeters":"-851","northernmostLatitude":"63.7622","southernmostLatitude":"63.7622","westernmostLongitude":"5.2553"}},"locationName":"Ocean>Atlantic Ocean>North Atlantic Ocean>Norwegian Sea","mappable":"Y","paleoData":[{"NOAADataTableId":"19706","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>paleocean>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/sejrup2010/sejrup2010.txt","linkText":"sejrup2010.txt","urlDescription":"Original Data and Full Metadata","variables":[{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"centimeter","cvWhat":"depth variable>depth"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"year Common Era","cvWhat":"age variable>age"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>foraminifer>planktic foraminifer>Neogloboquadrina sp.>Neogloboquadrina pachyderma","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"per mil","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"}]},{"NOAAKeywords":["earth science>paleoclimate>paleocean>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/sejrup2010/sejrup2010.xls","linkText":"sejrup2010.xls","urlDescription":"Original Data and Full Metadata","variables":[]}],"dataTableName":"P1-003SC","dataTableNotes":null,"earliestYear":991,"earliestYearBP":959,"earliestYearCE":991,"mostRecentYear":1665,"mostRecentYearBP":285,"mostRecentYearCE":1665,"species":[],"timeUnit":"AD"},{"NOAADataTableId":"19707","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>paleocean>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/sejrup2010/sejrup2010.txt","linkText":"sejrup2010.txt","urlDescription":"Original Data and Full Metadata","variables":[{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"centimeter","cvWhat":"depth variable>depth"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"year Common Era","cvWhat":"age variable>age"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>foraminifer>planktic foraminifer>Neogloboquadrina sp.>Neogloboquadrina pachyderma","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"per mil","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"}]},{"NOAAKeywords":["earth science>paleoclimate>paleocean>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/sejrup2010/sejrup2010.xls","linkText":"sejrup2010.xls","urlDescription":"Original Data and Full Metadata","variables":[]}],"dataTableName":"P1-003MC","dataTableNotes":null,"earliestYear":1241,"earliestYearBP":709,"earliestYearCE":1241,"mostRecentYear":1998,"mostRecentYearBP":-48,"mostRecentYearCE":1998,"species":[],"timeUnit":"AD"}],"siteName":"P1-003SC"}],"studyCode":null,"studyName":"Norwegian Sea P1-003MC/SC 1000 Year Planktonic d18O Data ","studyNotes":"High resolution (2.5-10 years) planktonic foraminifer oxygen isotope \nrecord from the Storegga Slide area, Norwegian Sea, for the past 1000 \nyears.  Oxygen isotope (d18O) measurements were made on the planktonic \nforaminifer Neogloboquadrina pachyderma (dextral form). \n\nMulticore P1-003MC (41.6 cm long) and core P1-003SC (~6m long) \nwere retrieved from the same location: ","version":"1.0","xmlId":"9572"}