Two centuries temperature variations over subtropical southeast China inferred from Pinus taiwanensis Hayata tree-ring width
文献类型：期刊论文
| 作者 | Cai, QiuFang3; Liu, Yu1,2,3 |
| 刊名 | CLIMATE DYNAMICS
 |
| 出版日期 | 2017-03-01 |
| 卷号 | 48期号:5-6页码:1813-1825 |
| 关键词 | Subtropical Southeast China Tree-ring Width Maximum Temperature Reconstruction Spatial Representativeness North Pacific Ocean Pdo |
| DOI | 10.1007/s00382-016-3174-8 |
| 文献子类 | Article |
| 英文摘要 | High-resolution long-term temperature reconstructions in subtropical southeast China (SSC) are very scarce, yet indispensable for the comprehensive understanding of climate change in China, even in East Asia. We reconstructed the first previous growth-season temperature in the Sanqingshan Mountains (SQS), southeast China since 1806 based on tree-ring width data. The reconstruction accounts for 56.4 % of the total variance in the instrumental record over 1954-2009. Unlike the Northern Hemispheric warming during recent two centuries, the reconstruction captured a slowly cooling trend from 1806 to 1980, followed by a rapid warming afterward. 2003-2009 was the warmest period in the reconstruction. 1970-2000 was colder than the last stage of the Little Ice Age (LIA). Most of the warm and cold periods in this reconstruction could be found in the tree-ring based temperature reconstructions of vicinity area, indicating that the temperature variations in SSC were almost synchronous at least at decadal scale. This regional coherence of temperature variation was further confirmed by the spatial correlation patterns with the CRU TS3.22 grid dataset. A strong positive relationship between the temperature over SQS region and sea surface temperature (SST) over the North Pacific Ocean (NP) has been noted, suggesting that SST variations over NP and the related Pacific Decadal Oscillation significantly influenced the temperature variability over SSC. To better understand the climate variability during the LIA and the regional differences in temperature variations over SQS and northern Hemisphere, long data sets from more diverse areas of southern China are needed. |
| WOS关键词 | NORTHERN-HEMISPHERE TEMPERATURE ; PACIFIC DECADAL OSCILLATION ; EASTERN TIBETAN PLATEAU ; SEA-SURFACE TEMPERATURE ; WESTERN HIMALAYA ; HALF CENTURIES ; YANGTZE-RIVER ; ICE-AGE ; VARIABILITY ; RECONSTRUCTION |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000395060900024 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5502]  |
| 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, Dept Environm Sci & Technol, Sch Human Settlements & Civil Engn, Xian 710049, Peoples R China 2.Beijing Normal Univ, JCGCS, Beijing 100875, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China |
| 推荐引用方式 GB/T 7714 | Cai, QiuFang,Liu, Yu. Two centuries temperature variations over subtropical southeast China inferred from Pinus taiwanensis Hayata tree-ring width[J]. CLIMATE DYNAMICS,2017,48(5-6):1813-1825. |
| APA | Cai, QiuFang,&Liu, Yu.(2017).Two centuries temperature variations over subtropical southeast China inferred from Pinus taiwanensis Hayata tree-ring width.CLIMATE DYNAMICS,48(5-6),1813-1825. |
| MLA | Cai, QiuFang,et al."Two centuries temperature variations over subtropical southeast China inferred from Pinus taiwanensis Hayata tree-ring width".CLIMATE DYNAMICS 48.5-6(2017):1813-1825. |
入库方式： OAI收割
来源：地球环境研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。