{"xmlId":"2499","NOAAStudyId":"5805","studyName":"Climate Model Output, LGM with Modern Ocean Heat Transport","doi":"https://doi.org/10.25921/z374-tj29","uuid":"cb5a0aae-eef0-4b2d-b7b0-c6627cd08893","dataPublisher":"NOAA","contactInfo":{"type":"CONTACT INFORMATION","shortName":"DOC/NOAA/NESDIS/NCEI","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","address":"325 Broadway, E/NE31","city":"Boulder","state":"CO","postalCode":"80305-3328","country":"USA","dataCenterUrl":"https://www.ncei.noaa.gov/products/paleoclimatology","email":"paleo@noaa.gov","phone":"828-271-4800","fax":null,"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."},"dataType":"PALEOCLIMATIC MODELING","investigators":"Webb, R.S.","investigatorDetails":[{"firstName":"Robert","lastName":"Webb","initials":"R.S.","orcId":null}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/5805","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-model-5805.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-model-5805.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/modeling","studyCode":null,"scienceKeywords":null,"reconstruction":"N","contributionDate":"2003-11-14","entryId":"noaa-model-5805","earliestYearBP":18000,"mostRecentYearBP":17000,"earliestYearCE":-16050,"mostRecentYearCE":-15050,"publication":[{"author":{"name":"Webb, R.S., Rind, D.H., Lehman, S.J., Healy, R.J., and Sigman, D."},"pubYear":1997,"title":"Influence of ocean heat transports on climate of the Last Glacial Maximum","journal":"Nature","volume":"385","edition":null,"issue":null,"pages":"695-699","reportNumber":null,"citation":"Webb, R.S., Rind, D.H., Lehman, S.J., Healy, R.J., and Sigman, D. 1997. Influence of ocean heat transports on climate of the Last Glacial Maximum. Nature, 385, 695-699. doi: 10.1038/385695a0","type":"publication","identifier":{"type":"doi","id":"10.1038/385695a0","url":"http://dx.doi.org/10.1038/385695a0"},"abstract":"A series of climate simulations using an atmospheric general circulation model shows that maintaining ocean heat transport at close to present-day values, but with otherwise glacial boundary conditions, leads to an enhanced cooling, particularly in the tropics. This is in agreement with recent geochemical evidence from fossil corals, ground waters, and ice. Near-modern ocean heat transport may have been sustained in all ocean basins during the Last Glacial Maximum in order to balance the formation and export of Glacial North Atlantic Intermediate Water.","pubRank":"1"}],"site":[{"NOAASiteId":"22723","siteName":"Global","siteCode":null,"mappable":"N","locationName":"Geographic Region>Global","geo":{"geoType":"Feature","geometry":{"type":"POLYGON","coordinates":["-90","90","-180","180"]},"properties":{"southernmostLatitude":"-90","northernmostLatitude":"90","westernmostLongitude":"-180","easternmostLongitude":"180","minElevationMeters":null,"maxElevationMeters":null}},"paleoData":[{"dataTableName":"Webb1997","NOAADataTableId":"32599","earliestYear":18000,"mostRecentYear":17000,"timeUnit":"cal yr BP","earliestYearBP":18000,"mostRecentYearBP":17000,"earliestYearCE":-16050,"mostRecentYearCE":-15050,"coreLengthMeters":null,"dataTableNotes":null,"species":[],"dataFile":[{"fileUrl":"https://www.ncei.noaa.gov/pub/data/paleo/gcmoutput/published_data/webb1997/","urlDescription":"Data Folder","linkText":"Data Folder","variables":[{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"age variable>age","cvMaterial":null,"cvError":null,"cvUnit":"time unit>age unit>day of year","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"sampling metadata>latitude","cvMaterial":null,"cvError":null,"cvUnit":"angle unit>degree>degree north","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"earth system variable>circulation variable>transport variable>northward ocean heat transport","cvMaterial":null,"cvError":null,"cvUnit":"power unit>watt","cvSeasonality":"annual","cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"10^15 watts","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"earth system variable>temperature variable>temperature>air temperature>surface air temperature","cvMaterial":null,"cvError":null,"cvUnit":"temperature unit>degree Celsius","cvSeasonality":"annual","cvDetail":"anomalized","cvMethod":null,"cvAdditionalInfo":"anomaly from control","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"earth system variable>temperature variable>temperature>sea water temperature>sea surface temperature","cvMaterial":null,"cvError":null,"cvUnit":"temperature unit>degree Celsius","cvSeasonality":"annual","cvDetail":"anomalized","cvMethod":null,"cvAdditionalInfo":"anomaly from control","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"earth system variable>energy variable>energy flux variable>radiative flux variable>planetary albedo","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":"annual","cvDetail":"anomalized","cvMethod":null,"cvAdditionalInfo":"anomaly from control","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"earth system variable>cryospheric variable>cryospheric quantity>sea ice cover","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":"annual","cvDetail":"anomalized","cvMethod":null,"cvAdditionalInfo":"anomaly from control","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCLIMATIC MODELING","cvWhat":"earth system variable>hydroclimatic variable>hydroclimate rate>evaporation","cvMaterial":null,"cvError":null,"cvUnit":"rate unit>length per time unit>millimeter per day","cvSeasonality":"annual","cvDetail":"anomalized","cvMethod":null,"cvAdditionalInfo":"anomaly from control; ocean evaporation","cvFormat":"Numeric","cvShortName":null}],"NOAAKeywords":["earth science>paleoclimate>model"]}]}]}],"reference":{"pastThesaurusSkos":"https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf","pastThesaurusExplorer":"https://www.ncei.noaa.gov/access/paleo-search/cvterms","gcmdKeywordThesaurus":"https://earthdata.nasa.gov/earth-observation-data/find-data/idn/gcmd-keywords"},"dataLicenseDescription":null,"dataLicenseUrl":null}