A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand

Abstract. Lumyai P, Palakit K, Suangsathaporn K, Wanthongchai K. 2020. A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand. Biodiversitas 21: 3938-3945. The objective of this study was to investigate the relationship between the growth of Pin...

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Autores principales:	Pichit Lumyai, KRITSADAPAN PALAKIT, KHWANCHAI DUANGSATHAPORN, KOBSAK WANTHONGCHAI
Formato:	article
Lenguaje:	EN
Publicado:	MBI & UNS Solo 2020
Materias:	chiang mai, highland, pinus latteri, temperature reconstructions, thailand Biology (General) QH301-705.5
Acceso en línea:	https://doaj.org/article/2ef787edae204969a329fbc435bdd27b
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spelling	oai:doaj.org-article:2ef787edae204969a329fbc435bdd27b2021-11-22T00:41:43ZA 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand1412-033X2085-472210.13057/biodiv/d210903https://doaj.org/article/2ef787edae204969a329fbc435bdd27b2020-08-01T00:00:00Zhttps://smujo.id/biodiv/article/view/6178https://doaj.org/toc/1412-033Xhttps://doaj.org/toc/2085-4722Abstract. Lumyai P, Palakit K, Suangsathaporn K, Wanthongchai K. 2020. A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand. Biodiversitas 21: 3938-3945. The objective of this study was to investigate the relationship between the growth of Pinus latteri and climate data in Chiang Mai Province, Thailand. Dendrochronological techniques were used to analyze 35 sample cores. The cross dated ring width data could be extended back for up to 324 years (1692-2015). The relationship between ring-width index and climate data indicated a significant correlation (p < 0.01) with the monthly rainfall in January, monthly temperature in August and September, extreme maximum temperature in August and mean maximum temperature in March and August. The reconstructed average monthly temperature in August was estimated at around 27.35 °C, a warming period could have occurred in 1694-1702, 1834-1844, 1848-1866, 1873-1876, 1884-1890, 1896-1902, 1911-1927, 1942-1958, and 1986-1990, with cooling periods occurring in 1703-1722, 1739-1752, 1865-1872, 1877-1883, 1891-1895, 1903-1910, 1928-1941, 1959-1961, and 1968-1970, which could explain the high fluctuations in temperature. Periods in the range 2.1-2.5, 10.1 , and 13.5 years were found to be common with the variations in El Niño-Southern Oscillation. In conclusion, the pine growth information can be used to monitor the variations in climate in Thailand.Pichit LumyaiKRITSADAPAN PALAKITKHWANCHAI DUANGSATHAPORNKOBSAK WANTHONGCHAIMBI & UNS Soloarticlechiang mai, highland, pinus latteri, temperature reconstructions, thailandBiology (General)QH301-705.5ENBiodiversitas, Vol 21, Iss 9 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	chiang mai, highland, pinus latteri, temperature reconstructions, thailand Biology (General) QH301-705.5
spellingShingle	chiang mai, highland, pinus latteri, temperature reconstructions, thailand Biology (General) QH301-705.5 Pichit Lumyai KRITSADAPAN PALAKIT KHWANCHAI DUANGSATHAPORN KOBSAK WANTHONGCHAI A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand
description	Abstract. Lumyai P, Palakit K, Suangsathaporn K, Wanthongchai K. 2020. A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand. Biodiversitas 21: 3938-3945. The objective of this study was to investigate the relationship between the growth of Pinus latteri and climate data in Chiang Mai Province, Thailand. Dendrochronological techniques were used to analyze 35 sample cores. The cross dated ring width data could be extended back for up to 324 years (1692-2015). The relationship between ring-width index and climate data indicated a significant correlation (p < 0.01) with the monthly rainfall in January, monthly temperature in August and September, extreme maximum temperature in August and mean maximum temperature in March and August. The reconstructed average monthly temperature in August was estimated at around 27.35 °C, a warming period could have occurred in 1694-1702, 1834-1844, 1848-1866, 1873-1876, 1884-1890, 1896-1902, 1911-1927, 1942-1958, and 1986-1990, with cooling periods occurring in 1703-1722, 1739-1752, 1865-1872, 1877-1883, 1891-1895, 1903-1910, 1928-1941, 1959-1961, and 1968-1970, which could explain the high fluctuations in temperature. Periods in the range 2.1-2.5, 10.1 , and 13.5 years were found to be common with the variations in El Niño-Southern Oscillation. In conclusion, the pine growth information can be used to monitor the variations in climate in Thailand.
format	article
author	Pichit Lumyai KRITSADAPAN PALAKIT KHWANCHAI DUANGSATHAPORN KOBSAK WANTHONGCHAI
author_facet	Pichit Lumyai KRITSADAPAN PALAKIT KHWANCHAI DUANGSATHAPORN KOBSAK WANTHONGCHAI
author_sort	Pichit Lumyai
title	A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand
title_short	A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand
title_full	A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand
title_fullStr	A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand
title_full_unstemmed	A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand
title_sort	324-years temperature reconstruction from pinus latteri mason at highland in chiang mai province, thailand
publisher	MBI & UNS Solo
publishDate	2020
url	https://doaj.org/article/2ef787edae204969a329fbc435bdd27b
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A 324-years temperature reconstruction from Pinus latteri Mason at highland in Chiang Mai Province, Thailand

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