A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand

A 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 sig...

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Main Authors: Chenxi Xu, Nathsuda Pumijumnong, Takeshi Nakatsuka, Masaki Sano, Zhen Li, นาฎสุดา ภูมิจำนงค์
Other Authors: Mahidol University. Faculty of Environment and Resource Studies.
Format: Article
Language:English
Published: 2016
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Online Access:https://repository.li.mahidol.ac.th/handle/123456789/48399
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Language: English
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spelling th-mahidol.483992023-04-12T15:24:32Z A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand Chenxi Xu Nathsuda Pumijumnong Takeshi Nakatsuka Masaki Sano Zhen Li นาฎสุดา ภูมิจำนงค์ Mahidol University. Faculty of Environment and Resource Studies. Research Institute for Humanity and Nature Nagoya University. Graduate School of Environment Studies. Tree-ring cellulose oxygen isotope Pinus merkusii Precipitation reconstruction ENSO A 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. 2016-02-27T08:13:02Z 2019-12-16T02:07:02Z 2016-02-27T08:13:02Z 2019-12-16T02:07:02Z 2016-02-26 2015-10 Article Journal of Hydrology. Vol.259, No.P2 (2015), 433-441. 10.1016/j.jhydrol.2015.02.037 0022-1694 https://repository.li.mahidol.ac.th/handle/123456789/48399 eng Mahidol University. Elsevier
institution Mahidol University
building Mahidol University Library
continent Asia
country Thailand
Thailand
content_provider Mahidol University Library
collection Mahidol University Institutional Repository
language English
topic Tree-ring cellulose oxygen isotope
Pinus merkusii
Precipitation reconstruction
ENSO
spellingShingle Tree-ring cellulose oxygen isotope
Pinus merkusii
Precipitation reconstruction
ENSO
Chenxi Xu
Nathsuda Pumijumnong
Takeshi Nakatsuka
Masaki Sano
Zhen Li
นาฎสุดา ภูมิจำนงค์
A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand
description A 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.
author2 Mahidol University. Faculty of Environment and Resource Studies.
author_facet Mahidol University. Faculty of Environment and Resource Studies.
Chenxi Xu
Nathsuda Pumijumnong
Takeshi Nakatsuka
Masaki Sano
Zhen Li
นาฎสุดา ภูมิจำนงค์
format Article
author Chenxi Xu
Nathsuda Pumijumnong
Takeshi Nakatsuka
Masaki Sano
Zhen Li
นาฎสุดา ภูมิจำนงค์
author_sort Chenxi Xu
title A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand
title_short A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand
title_full A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand
title_fullStr A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand
title_full_unstemmed A tree-ring cellulose d18O-based July–October precipitation reconstruction since AD 1828, northwest Thailand
title_sort tree-ring cellulose d18o-based july–october precipitation reconstruction since ad 1828, northwest thailand
publishDate 2016
url https://repository.li.mahidol.ac.th/handle/123456789/48399
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