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

##plugins.themes.bootstrap3.article.main##

PICHIT LUMYAI
KRITSADAPAN PALAKIT
KHWANCHAI DUANGSATHAPORN
KOBSAK WANTHONGCHAI

Abstract

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.

##plugins.themes.bootstrap3.article.details##

References
Buajan S, Pumijumnong N, Li Q, Liu Y. 2016. Oxygen isotope of teak tree-rings in North-West Thailand. Journal of Tropical Forest Science 28: 396–405.
Buckley B.M., M. Barbetti, M. Watanasak, R. D’Arrigo, S. Boonchirdchoo and S. Saratunon. 1995. Dendrochronological investigations in Thailand. IAWA 16: 393–409.
Buckley BM, Duangsathaporn K, Palakit K, Butler S, Syhapanya V, Xaybouangeun N. 2007. Analyses of growth rings of Pinus merkusii from Lao P.D.R. Forest Ecology and Management 253: 120-127.
Cook ER. 1985. A Time Series Analysis Approach to Tree-Ring Standardization. Ph.D. dissertation, University of Arizona.
Cook ER, Kairiukstis LA. 1990. Methods of Dendrochronology. Kluwer, Dordrecht.
D’Arrigo R, Barbetti M, Watanasak M, Buckley BM, Krusic PJ, Boonchirdchoo S, Sarutanon S. 1997. Progress in dendroclimatic studies of Mountain pine in Northern Thailand. IAWA Journal 18: 433–444.
Duangsathaporn K, Palakit K. 2013. Climatic Signals Derived from the Growth Variation and Cycles of Pinus merkusii in Easternmost Thailand. Thai Journal of Forestry 32(1): 9-23.
Fritts HC. 1976. Tree Ring and Climate. Academic Press, San Francisco.
Holmes RL. 1983. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull. 43: 69–78.
Hutameta A, Pumijumnong N. 2003. Pine tree-ring response to climate and ENSO at Ban Wat Chan, Chiang Mai. Environment and Natural Resources 1(2): 69-76.
Lumyai P, Duangsathporn K. 2017a. Pine growth variation and climate change: Opportunities for dendroclimatology in central Thailand. Journal of Tropical Forest Research 1: 23–35.
Lumyai, P, Duangsathaporn K. 2017b. Climate Reconstruction on the Growth of Teak in Umphang Wildlife Sanctuary, Thailand. Environment and Natural Resources Journal 16: 21–30.
Muangsong C, Cai B, Pumijumnong N, Hu C, Lei G. 2016. Intra-seasonal variability of teak tree-ring cellulose ?18O from northwestern Thailand: A potential proxy of Thailand summer monsoon rainfall. The Holocene 26: 1397–1405.
Northern Silvicultural Research Center. 2019. 50 years Pine. Northern Silvicultural Research Center Devision of Research Forest Research and Development office Royal Forest Department, Bangkok.
Palakit K, Duangsathaporn K, Siripatanadilok S. 2016. Climatic fluctuations trigger false ring occurrence and radial-growth variation in teak (Tectona grandis L.f.). iForest - Biogeosciences and Forestry 9: e1-e8.
Palakit K, Duangsathaporn K, Siripatanadilok S, Lumyai P. 2015. Effects of Climate Variability on Monthly Growth of Aglaia odoratissima and Hydnocarpus ilicifolia at the Sakaerat Environmental Research Station (SERS), Northeastern Thailand. Environment and Natural Resources Journal 13: 1–12.
Pumijumnong N, Wanyaphet T. 2006. Seasonal cambial activity and tree-ring formation of Pinus merkusii and Pinus kesiya in northern Thailand in dependence on climate. Forest Ecology and Management 226: 279–289.
Wat Chan Royal Project Development Center. 2019. Wat Chan Royal Project Development Center. http://royalprojectthailand.com/sites/default/files/WatChan-Eng_0.pdf.
Rakthai S, Fu PL, Fan ZX, Gaire NP, Pumijumnong N, Eiadthong W, Tangmitcharoen S. 2020. Increased Drought Sensitivity Results in a Declining Tree Growth of Pinus latteri in Northeastern Thailand. Forests 11: 2-18
Stokes MA, Smiley TL. 1968. An Introduction to Tree-Ring Dating. University of Chicago Press, Chicago.Journal:
Susatya, A, Yansen, Y. 2016. Dendrochronology of young Swietenia macrophylla and the variation of its growth response to the past wet climate in Bengkulu, Indonesia. Biodiversitas 17(2): 446-472.
Yordtong K, Duangsathaporn K Palakit K, , (2019) Climatic Factors on Growth of Pinus latteri Mason in Hill Evergreen Forest
at Phu Kradueng National Park, Loei Province. Thai Journal. Forestry.38(2): 124-135.

Most read articles by the same author(s)