Tree-ring stable carbon isotope-based June-September maximum temperature reconstruction since AD 1788, north-west Thailand
文献类型:期刊论文
作者 | Li, Qiang3; Payomrat, Paramate2,3; Liu, Yu1,3; Pumijumnong, Nathsuda4; Song, Huiming3 |
刊名 | TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY |
出版日期 | 2018-03-12 |
卷号 | 70期号:1443655 |
关键词 | North-west Thailand Tree-ring Cellulose Carbon Isotope Pinus Merkusii Maximum Temperature |
DOI | 10.1080/16000889.2018.1443655 |
文献子类 | Article |
英文摘要 | The 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. |
WOS关键词 | PINUS-MERKUSII ; INDIAN-OCEAN ; CLIMATE ; VARIABILITY ; CHINA ; ENSO ; CHRONOLOGIES ; DELTA-O-18 ; DELTA-C-13 ; CELLULOSE |
WOS研究方向 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS记录号 | WOS:000428085400001 |
源URL | [http://ir.ieecas.cn/handle/361006/5199] |
专题 | 地球环境研究所_现代环境研究室 |
作者单位 | 1.Xi An Jiao Tong Univ, Sch Human Settlements & Civil Engn, Dept Earth & Environm Sci, Xian, Shaanxi, Peoples R China 2.Univ Chinese Acad Sci, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Shaanxi, Peoples R China 4.Mahidol Univ, Fac Environm & Resource Studies, Salaya, Nakhon Pathom, Thailand |
推荐引用方式 GB/T 7714 | Li, Qiang,Payomrat, Paramate,Liu, Yu,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 | Li, Qiang,Payomrat, Paramate,Liu, Yu,Pumijumnong, Nathsuda,&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 | Li, Qiang,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). |
入库方式: OAI收割
来源:地球环境研究所
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