{"xmlId":"74192","NOAAStudyId":"32514","studyName":"Tibetan Plateau and Arctic 1,120 Year Temperature Reconstructions","doi":"https://doi.org/10.25921/sfpd-qk93","uuid":"a505729c-2a89-4372-a69a-ac66b3580b7a","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":"Shi, F.; Duan, A.; Yin, Q.; Bruun, J.T.; Xiao, C.; Guo, Z.","investigatorDetails":[{"firstName":"Feng","lastName":"Shi","initials":"F.","orcId":"0000-0003-3963-1822"},{"firstName":"Anmin","lastName":"Duan","initials":"A.","orcId":null},{"firstName":"Qiuzhen","lastName":"Yin","initials":"Q.","orcId":"0000-0002-7189-8335"},{"firstName":"John","lastName":"Bruun","initials":"J.T.","orcId":null},{"firstName":"Cunde","lastName":"Xiao","initials":"C.","orcId":null},{"firstName":"Zhengtang","lastName":"Guo","initials":"Z.","orcId":"0000-0003-2259-9715"}],"version":"1.0","funding":[],"studyNotes":"Annual temperature anomaly reconstructions for the Tibetan Plateau and the Arctic for the past 1,120 years.","onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/32514","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-recon-32514.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-recon-32514.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/climate-reconstruction","studyCode":null,"scienceKeywords":["Air Temperature Reconstruction"],"reconstruction":"Y","contributionDate":"2021-04-08","entryId":"noaa-recon-32514","earliestYearBP":1050,"mostRecentYearBP":-69,"earliestYearCE":900,"mostRecentYearCE":2019,"publication":[{"author":{"name":"Feng Shi, Anmin Duan, Qiuzhen Yin, John T. Bruun, Cunde Xiao, Zhengtang Guo"},"pubYear":2021,"title":"Modulation of the relationship between summer temperatures in the QinghaiTibetan Plateau and Arctic over the past millennium by external forcings","journal":"Quaternary Research","volume":null,"edition":"QUA-20-89R2","issue":null,"pages":null,"reportNumber":null,"citation":"Feng Shi, Anmin Duan, Qiuzhen Yin, John T. Bruun, Cunde Xiao, Zhengtang Guo. 2021. Modulation of the relationship between summer temperatures in the QinghaiTibetan Plateau and Arctic over the past millennium by external forcings. Quaternary Research. , QUA-20-89R2. doi: 10.1017/qua.2021.3","type":"publication","identifier":{"type":"doi","id":"10.1017/qua.2021.3","url":"http://dx.doi.org/10.1017/qua.2021.3"},"abstract":"The Qinghai-Tibetan Plateau and Arctic both have an important influence on global climate, but the correlation between climate variations in these two regions remains unclear. Here we reconstructed and compared the summer temperature anomalies over the past 1,120 yr (900-2019 CE) in the Qinghai-Tibetan Plateau and Arctic. The temperature correlation during the past millennium in these two regions has a distinct centennial variation caused by volcanic eruptions. Furthermore, the abrupt weak-to-strong transition in the temperature correlation during the sixteenth century could be analogous to this type of transition during the Modern Warm Period. The former was forced by volcanic eruptions, while the latter was controlled by changes in greenhouse gases. This implies that anthropogenic, as opposed to natural, forcing has acted to amplify the teleconnection between the Qinghai-Tibetan Plateau and Arctic during the Modern Warm Period.","pubRank":"1"}],"site":[{"NOAASiteId":"54080","siteName":"Arctic","siteCode":null,"mappable":"N","locationName":"Geographic 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