Chenxi XuNathsuda PumijumnongTakeshi NakatsukaMasaki SanoZhen Liนาฎสุดา ภูมิจำนงค์Mahidol University. Faculty of Environment and Resource Studies.Research Institute for Humanity and NatureNagoya University. Graduate School of Environment Studies.2016-02-272019-12-162016-02-272019-12-162016-02-262015-10Journal of Hydrology. Vol.259, No.P2 (2015), 433-441.0022-1694https://repository.li.mahidol.ac.th/handle/20.500.14594/48399A tree-ring d18O 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 d18O correlations were high during the entire period (r = 0.57–0.79). The tree-ring d18O 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 d18O chronology from living Pinus kesiya in northwest Thailand. The spatial correlation analysis between tree-ring d18O and regional July–October precipitation also support that the tree-ring d18O of P. merkusii is a promising proxy to reconstruct precipitation in northwest Thailand. The tree-ring d18O-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.engMahidol University.Tree-ring cellulose oxygen isotopePinus merkusiiPrecipitation reconstructionENSOArticleElsevier10.1016/j.jhydrol.2015.02.037