{"xmlId":"72532","NOAAStudyId":"30835","studyName":"Windy Lake Holocene Surface Air Temperature Reconstructions","doi":"https://doi.org/10.25921/78yg-ft28","uuid":"791ea2d8-5f11-4995-b343-31c962a1a9e3","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":"CLIMATE RECONSTRUCTIONS","investigators":"Chase, M.; Bleskie, C.; Walker, I.R.; Gavin, D.G.; Hu, F.S.","investigatorDetails":[{"firstName":"Marianne","lastName":"Chase","initials":"M.","orcId":null},{"firstName":"Christina","lastName":"Bleskie","initials":"C.","orcId":null},{"firstName":"Ian","lastName":"Walker","initials":"I.R.","orcId":null},{"firstName":"Daniel","lastName":"Gavin","initials":"D.G.","orcId":"0000-0001-8743-3949"},{"firstName":"Feng Sheng","lastName":"Hu","initials":"F.S.","orcId":null}],"version":"1.0","funding":[],"studyNotes":"This dataset was contributed as part of the Temperature-12k project (https://doi.org/10.25921/4RY2-G808). Data were contributed to the project from the original data generators, who are listed in the Investigator field of this template file. Additional notes regarding the use of these data in the Temperature-12k project can be found in the LiPD file listed as an Online_Resource of this template file.","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/30835","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-recon-30835.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-recon-30835.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/climate-reconstruction","studyCode":null,"scienceKeywords":["Air Temperature Reconstruction"],"reconstruction":"Y","contributionDate":"2020-04-15","entryId":"noaa-recon-30835","earliestYearBP":13048,"mostRecentYearBP":507,"earliestYearCE":-11098,"mostRecentYearCE":1443,"publication":[{"author":{"name":"Kaufman, D., McKay, N., Routson, C., et al."},"pubYear":2020,"title":"A global database of Holocene paleotemperature records","journal":"Scientific Data","volume":"7","edition":null,"issue":null,"pages":null,"reportNumber":"115","citation":"Kaufman, D., McKay, N., Routson, C., et al. 2020. A global database of Holocene paleotemperature records. Scientific Data, 7, 115. doi: 10.1038/s41597-020-0445-3","type":"publication","identifier":{"type":"doi","id":"10.1038/s41597-020-0445-3","url":"http://dx.doi.org/10.1038/s41597-020-0445-3"},"abstract":null,"pubRank":"3"},{"author":{"name":"Daniel G. Gavin  Linda B. Brubaker  D. Noah Greenwald"},"pubYear":2013,"title":"Postglacial climate and firemediated vegetation change on the western Olympic Peninsula, Washington (USA)","journal":"Ecological Monographs","volume":"83","edition":null,"issue":"4","pages":"471-489","reportNumber":null,"citation":"Daniel G. Gavin  Linda B. Brubaker  D. Noah Greenwald. 2013. Postglacial climate and firemediated vegetation change on the western Olympic Peninsula, Washington (USA). Ecological Monographs, 83(4), 471-489. doi: 10.1890/12-1742.1","type":"publication","identifier":{"type":"doi","id":"10.1890/12-1742.1","url":"http://dx.doi.org/10.1890/12-1742.1"},"abstract":null,"pubRank":"2"},{"author":{"name":"Chase, Marianne; Bleskie, Christina; Walker, Ian R.; Gavin, Daniel G.; Hu, Feng Sheng"},"pubYear":2008,"title":"Midge-inferred Holocene summer temperatures in southeastern British Columbia, Canada","journal":"Palaeogeography, Palaeoclimatology, Palaeoecology","volume":"257","edition":null,"issue":"2-Jan","pages":"244-259","reportNumber":null,"citation":"Chase, Marianne; Bleskie, Christina; Walker, Ian R.; Gavin, Daniel G.; Hu, Feng Sheng. 2008. Midge-inferred Holocene summer temperatures in southeastern British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology, 257(2-Jan), 244-259. doi: 10.1016/j.palaeo.2007.10.020","type":"publication","identifier":{"type":"doi","id":"10.1016/j.palaeo.2007.10.020","url":"http://dx.doi.org/10.1016/j.palaeo.2007.10.020"},"abstract":"Using fossil midge stratigraphies, we inferred Holocene summer temperatures at three subalpine lakes in eastern British Columbia. The late-glacial sediment indicated cool conditions, with an abundance of Microspectra atrofasciata/radialis type fossils at Thunder Lake and Redmountain Lake, and Sergentia at Windy Lake. Sergentia and Tanytarsus lugens/Corynocera oliveri type were dominant in the early Holocene, together with Chironomus at Redmountain Lake. At Thunder and Windy lakes, the early Holocene was dominated by warm-adapted taxa such as Microtendipes. Quantitative midge-temperature inference models reconstruct a 4 to 8 °C rise in mean July air temperature for Windy and Thunder lakes at the Pleistocene/Holocene transition. Early-Holocene temperatures averaged 3 to 4 °C warmer than those extant today. In contrast, no long-term temperature trend was evident at Redmountain Lake. This site may not reflect actual trends in air temperature due to runoff from a persistent snow pack in the watershed. Comparison of midge and pollen data suggests an inverse relationship between summer temperature and precipitation through the middle to late Holocene.","pubRank":"1"}],"site":[{"NOAASiteId":"58478","siteName":"Windy Lake CA","siteCode":null,"mappable":"Y","locationName":"Continent>North America>Canada>British Columbia","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["49.8133","-117.8772"]},"properties":{"southernmostLatitude":"49.8133","northernmostLatitude":"49.8133","westernmostLongitude":"-117.8772","easternmostLongitude":"-117.8772","minElevationMeters":"1814","maxElevationMeters":"1814"}},"paleoData":[{"dataTableName":"Windy.Chase.2008","NOAADataTableId":"43559","earliestYear":13048,"mostRecentYear":507,"timeUnit":"cal yr 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