{"NOAAStudyId":"1861","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":"2000-07-01","dataPublisher":"NOAA","dataType":"CORALS AND SCLEROSPONGES","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/coral-sclerosponge","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-coral-1861.xml","doi":null,"earliestYearBP":200,"earliestYearCE":1750,"entryId":"noaa-coral-1861","funding":[],"investigators":"Felis, T.; Pätzold, J.; Loya, Y.; Fine, M.; Nawar, A.H.; Wefer, G.","mostRecentYearBP":-45,"mostRecentYearCE":1995,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/1861","originalSource":null,"publication":[{"abstract":null,"author":null,"citation":"Felis, T., G. Lohmann, H. Kuhnert, S.J. Lorenz, D. Scholz, J. Pätzold, S.A. Al-Rousan, and S.M. Al-Moghrabi. 2004. Increased seasonality in Middle East temperatures during the last interglacial period. Nature 429(6988):164-168.","edition":null,"identifier":null,"issue":null,"journal":"Nature","pages":null,"pubRank":"2","pubYear":2004,"reportNumber":null,"title":"Increased seasonality in Middle East temperatures during the last interglacial period","type":"publication","volume":null},{"abstract":null,"author":{"name":"Rimbu, N.; Lohmann, G.; Felis, T.; Pätzold, J"},"citation":"Rimbu, N.; Lohmann, G.; Felis, T.; Pätzold, J. 2001. Arctic Oscillation signature in a Red Sea coral. Geophysical Research Letters, 28(15). doi: 10.1029/2001GL013083","edition":null,"identifier":{"id":"10.1029/2001GL013083","type":"doi","url":"http://dx.doi.org/10.1029/2001GL013083"},"issue":"15","journal":"Geophysical Research Letters","pages":null,"pubRank":"3","pubYear":2001,"reportNumber":null,"title":"Arctic Oscillation signature in a Red Sea coral","type":"publication","volume":"28"},{"abstract":null,"author":{"name":"Rimbu, N.; Lohmann, G.; Felis, T.; PÃ¤tzold, J"},"citation":"Rimbu, N.; Lohmann, G.; Felis, T.; PÃ¤tzold, J. 2003. Shift in ENSO teleconnections recorded by a northern Red Sea coral. Journal of Climate, 16. doi: 10.1175/1520-0442-16.9.1414","edition":null,"identifier":{"id":"10.1175/1520-0442-16.9.1414","type":"doi","url":"http://dx.doi.org/10.1175/1520-0442-16.9.1414"},"issue":null,"journal":"Journal of Climate","pages":null,"pubRank":"4","pubYear":2003,"reportNumber":null,"title":"Shift in ENSO teleconnections recorded by a northern Red Sea coral","type":"publication","volume":"16"},{"abstract":"A 245-year coral oxygen isotope record from the northern Red Sea (Ras Umm Sidd/Egypt, ~28N) in bimonthly resolution is presented. The mean annual coral d18O signal apparently reflects varying proportions of both sea surface temperature and d18Oseawater variability. In conjunction with instrumental observations of climate the coral record suggests for interannual and longer timescales that colder periods are accompanied by more arid conditions in the northern Red Sea but increased rainfall in the southeastern Mediterranean, whereas warmer periods are accompanied by decreased rainfall in the latter and less arid conditions in the northern Red Sea. A ~70-year oscillation of probably North Atlantic origin dominates the coral time series. Interannual to interdecadal variability is correlated with instrumental indices of the North Atlantic Oscillation (NAO), the El Nino-Southern Oscillation (ENSO), and North Pacific climate variability. The results suggest that these modes contributed consistently to Middle East climate variability since at least 1750, preferentially at a period of ~5.7 years.","author":{"name":"Thomas Felis, Jürgen Pätzold, Yossi Loya, Maoz Fine, Ahmed H. Nawar, Gerold Wefer"},"citation":"Thomas Felis, Jürgen Pätzold, Yossi Loya, Maoz Fine, Ahmed H. Nawar, Gerold Wefer. 2000. A coral oxygen isotope record from the northern Red Sea documenting NAO, ENSO, and North Pacific teleconnections on Middle East climate variability since the year 1750. Paleoceanography, 15(6), 679-694. doi: 10.1029/1999PA000477","edition":null,"identifier":{"id":"10.1029/1999PA000477","type":"doi","url":"http://dx.doi.org/10.1029/1999PA000477"},"issue":"6","journal":"Paleoceanography","pages":"679-694","pubRank":"1","pubYear":2000,"reportNumber":null,"title":"A coral oxygen isotope record from the northern Red Sea documenting NAO, ENSO, and North Pacific teleconnections on Middle East climate variability since the year 1750","type":"publication","volume":"15"}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"1864","geo":{"geoType":"Feature","geometry":{"coordinates":["27.848333","34.31"],"type":"POINT"},"properties":{"easternmostLongitude":"34.31","maxElevationMeters":"-6","minElevationMeters":"-6","northernmostLatitude":"27.848333","southernmostLatitude":"27.848333","westernmostLongitude":"34.31"}},"locationName":"Continent>Africa>Northern Africa>Egypt","mappable":"Y","paleoData":[{"NOAADataTableId":"1880","coreLengthMeters":3,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>corals and sclerosponges>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/coral/red_sea/felis2000_noaa.txt","linkText":"felis2000_noaa.txt","urlDescription":"Coral","variables":[{"cvAdditionalInfo":null,"cvDataType":"CORALS AND SCLEROSPONGES","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":"CORALS AND SCLEROSPONGES","cvDetail":"interpolated","cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>coral>Porites sp.","cvMethod":"isotope ratio mass spectrometry","cvSeasonality":null,"cvShortName":null,"cvUnit":"per mil VPDB","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"}]}],"dataTableName":"Ras Umm Sidd Core 001","dataTableNotes":null,"earliestYear":1750,"earliestYearBP":200,"earliestYearCE":1750,"mostRecentYear":1995,"mostRecentYearBP":-45,"mostRecentYearCE":1995,"species":[],"timeUnit":"AD"}],"siteName":"Ras Umm Sidd"}],"studyCode":null,"studyName":"Ras Umm Sidd - del18O Data ","studyNotes":null,"version":"1.0","xmlId":"1108"}