{"NOAAStudyId":"22413","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":"2017-07-10","dataPublisher":"NOAA","dataType":"PALEOLIMNOLOGY","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/lake","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-lake-22413.xml","doi":null,"earliestYearBP":6493,"earliestYearCE":-4543,"entryId":"noaa-lake-22413","funding":[{"fundingAgency":"Australian Research Council  ","fundingGrant":"LP0669104"},{"fundingAgency":"Australian Institute of Nuclear  Science and Engineering Research (AINSE)","fundingGrant":"AINGRA08124"}],"investigators":"Marx, S.K.; Kamber, B.A.; McGowan, H.A.; Denholm, J.","mostRecentYearBP":3,"mostRecentYearCE":1947,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/22413","originalSource":null,"publication":[{"abstract":null,"author":{"name":"Samuel K. Marx, Balz S. Kamber, Hamish A. McGowan, Atun Zawadzki"},"citation":"Samuel K. Marx, Balz S. Kamber, Hamish A. McGowan, Atun Zawadzki. 2010. Atmospheric pollutants in alpine peat bogs record a detailed chronology of industrial and agricultural development on the Australian continent. Environmental Pollution, 158(5), 1615-1628. doi: 10.1016/j.envpol.2009.12.009","edition":null,"identifier":{"id":"10.1016/j.envpol.2009.12.009","type":"doi","url":"http://dx.doi.org/10.1016/j.envpol.2009.12.009"},"issue":"5","journal":"Environmental Pollution","pages":"1615-1628","pubRank":"2","pubYear":2010,"reportNumber":null,"title":"Atmospheric pollutants in alpine peat bogs record a detailed chronology of industrial and agricultural development on the Australian continent","type":"publication","volume":"158"},{"abstract":"Millennial scale variability in the strength/position of the mid-latitude westerlies, as interpreted from rates of dust deposition in an alpine mire south-eastern Australia, is demonstrated to be a major driver of climate variability during the mid to late Holocene. Dust deposition rates were calculated with a trace element provenance model. This approach is capable of distinguishing between sedimentation of local alluvium and genuine deposition of aeolian dust into the studied mire. Low dust deposition from 6500 to 5500 cal. BP occurred during a period of enhanced south-westerly winds which advected moisture into south-eastern Australia resulting in wet conditions. A subsequent dust pulse at 5500-4000 cal. BP is interpreted as a relaxation in south-westerlies resulting in a more arid phase and possibly enhanced climate variability. Reduced dust deposition between 4000 and 2000 cal. BP indicates a return to increased precipitation/moisture in the lower MDB associated with increased south-westerly geostrophic flow. The onset of more arid conditions after 2000 cal. BP implies a reduction in the frequency of precipitation bearing south-westerly winds. A final further significant finding from this study is the identification of a major dust deposition/wind erosion episode coinciding with the onset of European land clearing and agriculture in Australia.","author":{"name":"Samuel K. Marx, Balz S. Kamber, Hamish A. McGowan, John Denholm"},"citation":"Samuel K. Marx, Balz S. Kamber, Hamish A. McGowan, John Denholm. 2011. Holocene dust deposition rates in Australia’s Murray-Darling Basin record the interplay between aridity and the position of the mid-latitude westerlies. Quaternary Science Reviews, 30(23-24), 3290-3305. doi: 10.1016/j.quascirev.2011.07.015","edition":null,"identifier":{"id":"10.1016/j.quascirev.2011.07.015","type":"doi","url":"http://dx.doi.org/10.1016/j.quascirev.2011.07.015"},"issue":"23-24","journal":"Quaternary Science Reviews","pages":"3290-3305","pubRank":"1","pubYear":2011,"reportNumber":null,"title":"Holocene dust deposition rates in Australia’s Murray-Darling Basin record the interplay between aridity and the position of the mid-latitude westerlies","type":"publication","volume":"30"}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"57365","geo":{"geoType":"Feature","geometry":{"coordinates":["-36.463","148.299"],"type":"POINT"},"properties":{"easternmostLongitude":"148.299","maxElevationMeters":"1940","minElevationMeters":"1940","northernmostLatitude":"-36.463","southernmostLatitude":"-36.463","westernmostLongitude":"148.299"}},"locationName":"Continent>Australia/New Zealand>Australia>New South Wales","mappable":"Y","paleoData":[{"NOAADataTableId":"33535","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>paleolimnology>physical properties"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/australia/snowy2011dust.txt","linkText":"Upper Snowy Mountains Dust Deposition Data","urlDescription":"Formatted Text Data File","variables":[{"cvAdditionalInfo":null,"cvDataType":"PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Character","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":null,"cvWhat":"sampling metadata>sample identification"},{"cvAdditionalInfo":null,"cvDataType":"PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"millimeter","cvWhat":"depth variable>depth"},{"cvAdditionalInfo":null,"cvDataType":"PALEOLIMNOLOGY","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":"PALEOLIMNOLOGY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"gram per square meter per year","cvWhat":"geological material>bulk geological material>dust"}]}],"dataTableName":"Snowy2011USCdust","dataTableNotes":null,"earliestYear":6493,"earliestYearBP":6493,"earliestYearCE":-4543,"mostRecentYear":3,"mostRecentYearBP":3,"mostRecentYearCE":1947,"species":[],"timeUnit":"cal yr BP"}],"siteName":"Upper Snowy Mountains"}],"studyCode":null,"studyName":"Upper Snowy Mountains, Australia 6,500 Year Dust Deposition Data","studyNotes":"Dust deposition rate from mire sediments collected in the Upper Snowy Range, New South Wales.","version":"1.0","xmlId":"20590"}