{"NOAAStudyId":"22051","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":"2017-03-14","dataPublisher":"NOAA","dataType":"LOESS","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/loess-eolian-dust","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-loess-22051.xml","doi":null,"earliestYearBP":13583,"earliestYearCE":-11633,"entryId":"noaa-loess-22051","funding":[{"fundingAgency":"National Natural Science Foundation China","fundingGrant":"41571178, 41371009"}],"investigators":"Li, Y.; Zhang, C.; Wang, Y.","mostRecentYearBP":0,"mostRecentYearCE":1950,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/22051","originalSource":null,"publication":[{"abstract":"Long-term changes of the Asian summer monsoon water vapor transport play a pivotal role in the variability of monsoon precipitation. Paleo-climate simulations have shown that there is an important monsoon vapor transport channel in western China. Previous studies mostly focused on the correlation between monsoon precipitation and intensity. Little research has been done on the verification of the water vapor channel. Compared with speleothem and lacustrine systems, the hydrological cycle of land surface sediments is more directly related to the monsoon water vapor. In this study, we used carbonate d18O and organic matter d13C of the surface eolian sediments from the piedmont of the northern Qilian Mountains to verify the monsoon water vapor on the Holocene millennial-scale. Two surface sedimentary sections were selected to study paleo-monsoon water vapor transport. Proxy data, including carbonate d18O and organic matter d13C of surface eolian sediments, as well as total organic matter and carbonate content were obtained from the two eolian sections. We also synthesized transient simulations of the CCSM3 and the Kiel climate models. The PMIP 3.0 project and TRACE isotopic simulations were also compared with the reconstructed monsoon water vapor transport. Our findings indicate that the strength of the Holocene Asian summer monsoon is consistent with the water vapor transport in western China that has significant impacts to long-term monsoon precipitation in northern China. This study verifies a significant millennial-scale correlation between the monsoon strength and monsoon water vapor transport intensity along the eastern Qinghai-Tibet Plateau.","author":{"name":"Yu Li, Chengqi Zhang, Yue Wang"},"citation":"Yu Li, Chengqi Zhang, Yue Wang. 2016. The verification of millennial-scale monsoon water vapor transport channel in northwest China. Journal of Hydrology, 536, 273-283. doi: 10.1016/j.jhydrol.2016.03.006","edition":null,"identifier":{"id":"10.1016/j.jhydrol.2016.03.006","type":"doi","url":"http://dx.doi.org/10.1016/j.jhydrol.2016.03.006"},"issue":null,"journal":"Journal of Hydrology","pages":"273-283","pubRank":"1","pubYear":2016,"reportNumber":null,"title":"The verification of millennial-scale monsoon water vapor transport channel in northwest China","type":"publication","volume":"536"}],"reconstruction":"N","scienceKeywords":["Monsoon"],"site":[{"NOAASiteId":"57161","geo":{"geoType":"Feature","geometry":{"coordinates":["37.4167","102.6"],"type":"POINT"},"properties":{"easternmostLongitude":"102.6","maxElevationMeters":"2447","minElevationMeters":"2447","northernmostLatitude":"37.4167","southernmostLatitude":"37.4167","westernmostLongitude":"102.6"}},"locationName":"Continent>Asia>Eastern Asia>China","mappable":"Y","paleoData":[{"NOAADataTableId":"33134","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth 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