{"NOAAStudyId":"6073","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":"2008-01-22","dataPublisher":"NOAA","dataType":"FIRE HISTORY","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/fire-history","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-fire-6073.xml","doi":null,"earliestYearBP":null,"earliestYearCE":null,"entryId":"noaa-fire-6073","funding":[],"investigators":"Power, M.J.; Marlon, J.","mostRecentYearBP":null,"mostRecentYearCE":null,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/6073","originalSource":null,"publication":[{"abstract":"Fire activity has varied globally and continuouslysince the last glacial maximum (LGM) in response tolong-term changes in global climate and shorter-termregional changes in climate, vegetation, and human landuse. We have synthesized sedimentary charcoal records ofbiomass burning since the LGM and present global mapsshowing changes in fire activity for time slices during thepast 21,000 years (as differences in charcoal accumulationvalues compared to pre-industrial). There is strong broadscalecoherence in fire activity after the LGM, but spatialheterogeneity in the signals increases thereafter. In NorthAmerica, Europe and southern South America, charcoalrecords indicate less-than-present fire activity during thedeglacial period, from 21,000 to ~11,000 cal yr BP. Incontrast, the tropical latitudes of South America and Africashow greater-than-present fire activity from ~19,000 to~17,000 cal yr BP and most sites from Indochina andAustralia show greater-than-present fire activity from16,000 to ~13,000 cal yr BP. Many sites indicate greaterthan-present or near-present activity during the Holocenewith the exception of eastern North America and easternAsia from 8,000 to ~3,000 cal yr BP, Indonesia andAustralia from 11,000 to 4,000 cal yr BP, and southernSouth America from 6,000 to 3,000 cal yr BP where fireactivity was less than present. Regional coherence in thepatterns of change in fire activity was evident throughoutthe post-glacial period. These complex patterns can largelybe explained in terms of large-scale climate controlsmodulated by local changes in vegetation and fuel load.","author":null,"citation":"Power, M.J., Marlon, J., Bartlein, P.J., Harrison, S.P., Mayle, F.E., Ballouche, A., Bradshaw, R., Carcaillet, C., Cordova, C., Mooney, S., Moreno, P., Prentice, I.C., Thonicke, K., Tinner, W., Whitlock, C., Zhang, Y., Zhao, Y., Anderson, R.S., Beer, R., Behling, H., Briles, C., Brown, K.J., Brunelle A., Bush, M., Camill, P., Chu, G.Q., Clark, J., Colombaroli, D., Connor, S., Daniels, M., Daniau, A.-L., Dodson, J., Doughty, E., Edwards, M.E., Fisinger, W., Foster, D., Frechette J., Gaillard, M.-J., Gil-Romera, G. Gavin, D.G., Gobet, E., Haberle, S., Hallett, D.J., Higuera, P., Hope, G., Horn, S., Impagliazzo, S., Inoue, J., Kaltenrieder, P., Kennedy, L., Kong, Z.C., Larsen, C., Long, C.J., Lynch, J., Lynch, B., McGlone, M., Meeks, S., Mensing, S., Meyer, G., Minckley, T., Mohr, J, Nelson, D., New, J., Newnham, R., Noti, R., Oswald, W., Pierce, J., Richard, P.J.H., Rowe, C., Sanchez Goņi, M.F., Shuman, B.J., Takahara, H., Toney, J., Turney, C.., Umbanhower, C., Vandergoes, M., Vanniere, B., Vescovi, E., Walsh, M., Wang, X., Williams, N., Wilmshurst, J., Zhang , J.H. 2008. Changes in fire regimes since the Last Glacial Maximum: an assessment based on a global synthesis and analysis of charcoal data. Climate Dynamics, Vol. 30, No. 7-8, pp. 887-907. DOI 10.1007/s00382-007-0334-x","edition":null,"identifier":{"id":"10.1007/s00382-007-0334-x","type":"doi","url":"http://dx.doi.org/10.1007/s00382-007-0334-x"},"issue":null,"journal":"Climate Dynamics","pages":null,"pubRank":"1","pubYear":2008,"reportNumber":null,"title":"Changes in fire regimes since the Last Glacial Maximum: an assessment based on a global synthesis and analysis of charcoal data","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"30718","geo":{"geoType":"Feature","geometry":{"coordinates":["37.177948","-119.02767"],"type":"POINT"},"properties":{"easternmostLongitude":"-119.02767","maxElevationMeters":"290","minElevationMeters":"230","northernmostLatitude":"37.177948","southernmostLatitude":"37.177948","westernmostLongitude":"-119.02767"}},"locationName":"Continent>North America>United States Of America","mappable":"Y","paleoData":[{"NOAADataTableId":"Unspecified","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>fire history>charcoal sediment"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/firehistory/charcoal/gcd/","linkText":"Data Folder","urlDescription":"Data Folder","variables":[]}],"dataTableName":null,"dataTableNotes":null,"earliestYear":null,"earliestYearBP":null,"earliestYearCE":null,"mostRecentYear":null,"mostRecentYearBP":null,"mostRecentYearCE":null,"species":[],"timeUnit":null}],"siteName":"East Lake - 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A description of the data \nis contained in this paper, and the complete citation is listed below. \nThese data are provided as-is. In some cases, data may be missing or may differ from \noriginally published data due to database entry, import and conversion methods. \nThese data were compiled by the \nGlobal Palaeofire Working Group (GPWG). \nPlease see their website for additional information on the development of the \nGPWG and the history of the database.","version":"1.0","xmlId":"693"}