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Please use this identifier to cite or link to this item: http://repository.li.mahidol.ac.th/dspace/handle/123456789/35984
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dc.contributor.authorChenxi Xuen_US
dc.contributor.authorNathsuda Pumijumnongen_US
dc.contributor.authorTakeshi Nakatsukaen_US
dc.contributor.authorMasaki Sanoen_US
dc.contributor.authorZhen Lien_US
dc.contributor.otherNational Institutes for the Humanities, Research Institute for Humanity and Natureen_US
dc.contributor.otherFaculty of Environment and Resource Studies, Mahidol Universityen_US
dc.contributor.otherNagoya Universityen_US
dc.date.accessioned2018-11-23T10:10:12Z-
dc.date.available2018-11-23T10:10:12Z-
dc.date.issued2015-10-01en_US
dc.identifier.citationJournal of Hydrology. Vol.529, No.P2 (2015), 433-441en_US
dc.identifier.issn00221694en_US
dc.identifier.other2-s2.0-84940953707en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84940953707&origin=inwarden_US
dc.identifier.urihttp://repository.li.mahidol.ac.th/dspace/handle/123456789/35984-
dc.description.abstract© 2015 Elsevier B.V. A tree-ring δ18O chronology for the period 1828-2000 was developed from four Pinus merkusii trees, to find a reliable proxy for reconstructing precipitation in northwest Thailand. Inter-tree δ18O correlations were high during the entire period (r=0.57-0.79). The tree-ring δ18O chronology shows significant negative correlations with regional July-October precipitation during the period 1901-2000 (r=-0.62) and with July-October river flow (r=-0.54), and is in good agreement with a shorter tree-ring δ18O chronology from living Pinus kesiya in northwest Thailand. The spatial correlation analysis between tree-ring δ18O and regional July-October precipitation also support that the tree-ring δ18O of P. merkusii is a promising proxy to reconstruct precipitation in northwest Thailand. The tree-ring δ18O-based July-October reconstruction, which accounts for 37.6% of the precipitation variance, shows a close relationship with El Niño-Southern Oscillation (ENSO) during the period 1871-2000, with the exception of during the past two decades; the exception may be related to the southeastward shift of the descending limb of Walker circulation and increased frequency of central Pacific ENSO.en_US
dc.rightsMahidol Universityen_US
dc.source.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84940953707&origin=inwarden_US
dc.subjectEnvironmental Scienceen_US
dc.titleA tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailanden_US
dc.typeArticleen_US
dc.rights.holderSCOPUSen_US
dc.identifier.doi10.1016/j.jhydrol.2015.02.037en_US
Appears in Collections:Scopus 2011-2015

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