{"NOAAStudyId":"2608","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":"2003-07-01","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-2608.xml","doi":null,"earliestYearBP":10848,"earliestYearCE":-8898,"entryId":"noaa-ocean-2608","funding":[],"investigators":"Friddell, J.E.; Thunell, R.C.; Guilderson, T.P.; Kashgarian, M.","mostRecentYearBP":837,"mostRecentYearCE":1113,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/2608","originalSource":null,"publication":[{"abstract":"We use a pair of decadally resolved planktonic foraminiferal d18O records from Santa Barbara Basin (SBB) to show that the warmest interval of the current interglacial, the middle Holocene, was characterized by increased decadal- to centennial-scale climatic variability. Modern relationships between the Pacific Decadal Oscillation (PDO), the El Niņo-Southern Oscillation (ENSO), and upper water conditions in SBB also suggest a preference of the northeast (NE) Pacific climate during the warm mid-Holocene toward the warm phase of the PDO and more intense ENSO warm events (\"\"El Niņos\"\"). In the context of future climate, this study suggests increasing decadal- to centennial-scale climatic variability in a globally warmed world.","author":null,"citation":"Friddell, J.E., R.C. Thunell, T.P. Guilderson, and M. Kashgarian. 2003. Increased northeast Pacific climatic variability during the warm middle Holocene. Geophysical Research Letters 30(11):1560.","edition":null,"identifier":null,"issue":null,"journal":"Geophysical Research Letters","pages":null,"pubRank":"1","pubYear":2003,"reportNumber":null,"title":"Increased northeast Pacific climatic variability during the warm middle Holocene","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"19238","geo":{"geoType":"Feature","geometry":{"coordinates":["34.27","-120.07"],"type":"POINT"},"properties":{"easternmostLongitude":"-120.07","maxElevationMeters":"-575","minElevationMeters":"-575","northernmostLatitude":"34.27","southernmostLatitude":"34.27","westernmostLongitude":"-120.07"}},"locationName":"Ocean>Pacific Ocean>North Pacific Ocean","mappable":"Y","paleoData":[{"NOAADataTableId":"4292","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>paleocean>oxygen isotopes","earth science>paleoclimate>paleocean>physical properties","earth science>paleoclimate>paleocean>age control"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/friddell2003","linkText":"friddell2003","urlDescription":"Original Data and Full Metadata","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>paleocean>physical properties","earth science>paleoclimate>paleocean>oxygen isotopes","earth science>paleoclimate>paleocean>age control"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/jpc76-f-tab.txt","linkText":"jpc76-f-tab.txt","urlDescription":"Alternate Format Data","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":"calendar year before present","cvWhat":"age variable>age"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"radiocarbon year before present","cvWhat":"age variable>age"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":"corrected","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":"biological material>organism>foraminifer>planktic foraminifer>Globigerina sp.>Globigerina bulloides","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"per mil PDB","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"},{"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 PDB","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"}]}],"dataTableName":"JPC76","dataTableNotes":"Depths below 486 cm have a corrected depth due to the presence of a foraminifera-poor sandy layer, interpreted as a turbidite, between 486 and 521 cm.","earliestYear":9522,"earliestYearBP":10848,"earliestYearCE":-8898,"mostRecentYear":907,"mostRecentYearBP":837,"mostRecentYearCE":1113,"species":[],"timeUnit":"14C yr BP"}],"siteName":"JPC76"}],"studyCode":null,"studyName":"Santa Barbara Basin Holocene Stable Oxygen Isotope Data ","studyNotes":null,"version":"1.0","xmlId":"1679"}