{"NOAAStudyId":"1883","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":"2004-07-01","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-1883.xml","doi":null,"earliestYearBP":121894,"earliestYearCE":-119944,"entryId":"noaa-coral-1883","funding":[],"investigators":"Felis, T.; Lohmann, G.; Kuhnert, H.; Lorenz, S.J.; Scholz, D.; Pätzold, J.; Al-Rousan, S.A.; Al-Moghrabi, S.M.","mostRecentYearBP":-46,"mostRecentYearCE":1996,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/1883","originalSource":null,"publication":[{"abstract":"The last interglacial period (about 125,000 years ago) is thought to have been at least as warm as the present climate. Owing to changes in the Earth's orbit around the Sun, it is thought that insolation in the Northern Hemisphere varied more strongly than today on seasonal timescales, which would have led to corresponding changes in the seasonal temperature cycle. Here we present seasonally resolved proxy records using corals from the northernmost Red Sea, which record climate during the last interglacial period, the late Holocene epoch and the present. We find an increased seasonality in the temperature recorded in the last interglacial coral. Today, climate in the northern Red Sea is sensitive to the North Atlantic Oscillation, a climate oscillation that strongly influences winter temperatures and precipitation in the North Atlantic region.  From our coral records and simulations with a coupled atmosphere-ocean circulation model, we conclude that a tendency towards the high-index state of the North Atlantic Oscillation during the last interglacial period, which is consistent with European proxy records, contributed to the larger amplitude of the seasonal cycle in the Middle East.","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":"1","pubYear":2004,"reportNumber":null,"title":"Increased seasonality in Middle East temperatures during the last interglacial period","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"1858","geo":{"geoType":"Feature","geometry":{"coordinates":["29.42","34.97"],"type":"POINT"},"properties":{"easternmostLongitude":"34.97","maxElevationMeters":"-4","minElevationMeters":"-4","northernmostLatitude":"29.42","southernmostLatitude":"29.42","westernmostLongitude":"34.97"}},"locationName":"Continent>Asia>Western Asia>Middle East>Jordan","mappable":"Y","paleoData":[{"NOAADataTableId":"1986","coreLengthMeters":3,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>corals and sclerosponges>trace metals","earth science>paleoclimate>corals and sclerosponges>oxygen 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