A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand

© 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 c...

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Main Authors: Chenxi Xu, Nathsuda Pumijumnong, Takeshi Nakatsuka, Masaki Sano, Zhen Li
Other Authors: National Institutes for the Humanities, Research Institute for Humanity and Nature
Format: Article
Published: 2018
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Online Access:https://repository.li.mahidol.ac.th/handle/123456789/35984
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spelling th-mahidol.359842018-11-23T17:10:12Z A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand Chenxi Xu Nathsuda Pumijumnong Takeshi Nakatsuka Masaki Sano Zhen Li National Institutes for the Humanities, Research Institute for Humanity and Nature Faculty of Environment and Resource Studies, Mahidol University Nagoya University Environmental Science © 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. 2018-11-23T10:10:12Z 2018-11-23T10:10:12Z 2015-10-01 Article Journal of Hydrology. Vol.529, No.P2 (2015), 433-441 10.1016/j.jhydrol.2015.02.037 00221694 2-s2.0-84940953707 https://repository.li.mahidol.ac.th/handle/123456789/35984 Mahidol University SCOPUS https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84940953707&origin=inward
institution Mahidol University
building Mahidol University Library
continent Asia
country Thailand
Thailand
content_provider Mahidol University Library
collection Mahidol University Institutional Repository
topic Environmental Science
spellingShingle Environmental Science
Chenxi Xu
Nathsuda Pumijumnong
Takeshi Nakatsuka
Masaki Sano
Zhen Li
A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand
description © 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.
author2 National Institutes for the Humanities, Research Institute for Humanity and Nature
author_facet National Institutes for the Humanities, Research Institute for Humanity and Nature
Chenxi Xu
Nathsuda Pumijumnong
Takeshi Nakatsuka
Masaki Sano
Zhen Li
format Article
author Chenxi Xu
Nathsuda Pumijumnong
Takeshi Nakatsuka
Masaki Sano
Zhen Li
author_sort Chenxi Xu
title A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand
title_short A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand
title_full A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand
title_fullStr A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand
title_full_unstemmed A tree-ring cellulose δ<sup>18</sup>O-based July-October precipitation reconstruction since AD 1828, northwest Thailand
title_sort tree-ring cellulose δ<sup>18</sup>o-based july-october precipitation reconstruction since ad 1828, northwest thailand
publishDate 2018
url https://repository.li.mahidol.ac.th/handle/123456789/35984
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