Kanokrat BuarealSupaporn BuajanSineenart PreechamartChotika MuangsongNathsuda PumijumnongFaculty of Environment and Resource Studies, Mahidol UniversityMahidol University2020-08-252020-08-252020-01-01Applied Environmental Research. Vol.42, No.1 (2020), 85-1002287075X228707412-s2.0-85084535471https://repository.li.mahidol.ac.th/handle/20.500.14594/57921© 2020, Chulalongkorn University - Environmental Research Institute. All rights reserved. Teak ring-width is one of the promising paleoclimate proxies in the tropical region. Tree-ring chronology spanning from 1840 to 2016 (177 years) was derived from 76 trees from Phrae Province, northern Thailand. A total of 141 core samples were cross-dated, a standardized master was constructed, and the tree residual master chronology was developed by ARSTAN program. The tree-ring chronology has a significant positive correlation with the monthly rainfall and relative humidity during the monsoon season (May–June). In addition, the growth of tree-ring width also significantly inversely correlated with Niño 3, Niño 3.4, and Niño 4 indices during the second half of the dry season (January–March). We reconstructed summer monsoon season (May–June) rainfall based on a linear regression model which explained 21.95% of the actual rainfall variance. The trend of the reconstructed rainfall record shows a decrease of 0.6 mm per decade and substantially showed four wet periods and five dry periods. These results suggest that this teak chronology has a good potential to be a high-resolution proxy for reconstructing the past local climate in northern Thailand.Mahidol UniversityEnvironmental ScienceArticleSCOPUS10.35762/AER.2020.42.1.7