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Tree-ring stable carbon isotope-based June-September maximum temperature reconstruction since AD 1788, north-west Thailand
Payomrat, Paramate1,2; Liu, Yu1,3; Pumijumnong, Nathsuda4; Li, Qiang1; Song, Huiming1
2018-03-12
Source PublicationTELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY
Volume70Issue:1443655
SubtypeArticle
AbstractThe first study of tree-ring stable carbon isotopes in Thailand has demonstrated that stable carbon isotope in northwestern Thailand represents a promising proxy for the temperature reconstruction of core-monsoon periods. A tree-ring delta C-13 chronology was constructed based on four cores covering the period of 1788-2013. After removing the long-term decreasing trend reflecting atmospheric CO2 concentrations, the Delta C-13 chronology was able to capture both temperature and hydro-climate signals Delta C-13 chronology showed particularly strong and significant negative correlation (r = -0.62, p < 0.0001) with June-September maximum temperature (CRU TS 3.24). The maximum temperature was reconstructed, which explained 37.8% of the variance in the instrumental maximum temperatures over the period of 1901-2013. The maximum temperature reconstruction revealed that four cooler and three warmer periods, as well as a slightly increasing temperature trend, occurred during the late seventeenth to mid-eighteenth centuries, which were followed by severe temperature fluctuations during the twentieth century century. While the sea surface temperature anomaly in the Indian Ocean might not affect the maximum temperature, its unstable relationship with the El Nino-Southern Oscillation (ENSO) was detected. In addition, a close relationship was observed between the maximum temperature and ENSO during the negative phase of the Pacific Decadal Oscillation (PDO), but this relationship was lost during the positive phase of the PDO.
KeywordNorth-west Thailand Tree-ring Cellulose Carbon Isotope Pinus Merkusii Maximum Temperature
WOS HeadingsScience & Technology ; Physical Sciences
DOI10.1080/16000889.2018.1443655
WOS KeywordPINUS-MERKUSII ; INDIAN-OCEAN ; CLIMATE ; VARIABILITY ; CHINA ; ENSO ; CHRONOLOGIES ; DELTA-O-18 ; DELTA-C-13 ; CELLULOSE
Indexed BySCI
Language英文
WOS Research AreaMeteorology & Atmospheric Sciences
WOS SubjectMeteorology & Atmospheric Sciences
WOS IDWOS:000428085400001
Citation statistics
Cited Times:1[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/5199
Collection现代环境研究室
Affiliation1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Shaanxi, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Xi An Jiao Tong Univ, Sch Human Settlements & Civil Engn, Dept Earth & Environm Sci, Xian, Shaanxi, Peoples R China
4.Mahidol Univ, Fac Environm & Resource Studies, Salaya, Nakhon Pathom, Thailand
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Payomrat, Paramate,Liu, Yu,Pumijumnong, Nathsuda,et al. Tree-ring stable carbon isotope-based June-September maximum temperature reconstruction since AD 1788, north-west Thailand[J]. TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY,2018,70(1443655).
APA Payomrat, Paramate,Liu, Yu,Pumijumnong, Nathsuda,Li, Qiang,&Song, Huiming.(2018).Tree-ring stable carbon isotope-based June-September maximum temperature reconstruction since AD 1788, north-west Thailand.TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY,70(1443655).
MLA Payomrat, Paramate,et al."Tree-ring stable carbon isotope-based June-September maximum temperature reconstruction since AD 1788, north-west Thailand".TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY 70.1443655(2018).
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