Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/19488
DC FieldValueLanguage
dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorWang, Y-
dc.creatorCheng, H-
dc.creatorEdwards, RL-
dc.creatorHe, Y-
dc.creatorKong, X-
dc.creatorAn, Z-
dc.creatorWu, J-
dc.creatorKelly, MJ-
dc.creatorDykoski, CA-
dc.creatorLi, X-
dc.date.accessioned2014-12-19T06:59:55Z-
dc.date.available2014-12-19T06:59:55Z-
dc.identifier.issn0036-8075-
dc.identifier.urihttp://hdl.handle.net/10397/19488-
dc.language.isoenen_US
dc.titleThe holocene Asian monsoon : links to solar changes and North Atlantic climateen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage854-
dc.identifier.epage857-
dc.identifier.volume308-
dc.identifier.issue5723-
dc.identifier.doi10.1126/science.1106296-
dcterms.abstractA 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years. Although the record broadly follows summer insolation, it is punctuated by eight weak monsoon events lasting ∼1 to 5 centuries. One correlates with the "8200-year" event, another with the collapse of the Chinese Neolithic culture, and most with North Atlantic ice-rafting events. Cross-correlation of the decadal- to centennial-scale monsoon record with the atmospheric carbon-14 record shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.-
dcterms.bibliographicCitationScience, 2005, v. 308, no. 5723, p. 854-857-
dcterms.isPartOfScience-
dcterms.issued2005-
dc.identifier.isiWOS:000228986500048-
dc.identifier.scopus2-s2.0-20944452270-
dc.identifier.rosgroupidr20786-
dc.description.ros2004-2005 > Academic research: refereed > Publication in refereed journal-
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