Climate Response of Tree Radial Growth at Different Timescales in the Qinling Mountains
文献类型：期刊论文
| 作者 | Sun, Changfeng1,2; Liu, Yu1,2 |
| 刊名 | PLOS ONE
 |
| 出版日期 | 2016-08-10 |
| 卷号 | 11期号:8 |
| DOI | 10.1371/journal.pone.0160938 |
| 文献子类 | Article |
| 英文摘要 | The analysis of the tree radial growth response to climate is crucial for dendroclimatological research. However, the response relationships between tree-ring indices and climatic factors at different timescales are not yet clear. In this study, the tree-ring width of Huashan pine (Pinus armandii) from Huashan in the Qinling Mountains, north-central China, was used to explore the response differences of tree growth to climatic factors at daily, pentad (5 days), dekad (10 days) and monthly timescales. Correlation function and linear regression analysis were applied in this paper. The tree-ring width showed a more sensitive response to daily and pentad climatic factors. With the timescale decreasing, the absolute value of the maximum correlation coefficient between the tree-ring data and precipitation increases as well as temperature (mean, minimum and maximum temperature). Compared to the other three timescales, pentad was more suitable for analysing the response of tree growth to climate. Relative to the monthly climate data, the association between the tree-ring data and the pentad climate data was more remarkable and accurate, and the reconstruction function based on the pentad climate was also more reliable and stable. We found that the major climatic factor limiting Huashan pine growth was the precipitation of pentads 20-35 (from April 6 to June 24) rather than the well-known April-June precipitation. The pentad was also proved to be a better timescale for analysing the climate and tree growth in the western and eastern Qinling Mountains. The formation of the earlywood density of Chinese pine (Pinus tabulaeformis) from Shimenshan in western Qinling was mainly affected by the maximum temperature of pentads 28-32 (from May 16 to June 9). The maximum temperature of pentads 28-33 (from May 16 to June 14) was the major factor affecting the ring width of Chinese pine from Shirenshan in eastern Qinling. |
| WOS关键词 | NORTHEASTERN TIBETAN PLATEAU ; NORTH-CENTRAL CHINA ; BALSAMEA L. MILL. ; INNER-MONGOLIA ; TEMPERATURE RECONSTRUCTION ; PRECIPITATION RECORDS ; PINUS-TABULAEFORMIS ; GROWING-SEASON ; EASTERN CHINA ; EARLY SUMMER |
| WOS研究方向 | Science & Technology - Other Topics |
| 语种 | 英语 |
| WOS记录号 | WOS:000381380400068 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5689]  |
| 专题 | 地球环境研究所_现代环境研究室 |
| 作者单位 | 1.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, 97 Yanxiang Rd, Xian 710061, Peoples R China 2.Xi An Jiao Tong Univ, Dept Earth & Environm Sci, Sch Human Settlements & Civil Engn, 28 Xianning West Rd, Xian 710049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Sun, Changfeng,Liu, Yu. Climate Response of Tree Radial Growth at Different Timescales in the Qinling Mountains[J]. PLOS ONE,2016,11(8). |
| APA | Sun, Changfeng,&Liu, Yu.(2016).Climate Response of Tree Radial Growth at Different Timescales in the Qinling Mountains.PLOS ONE,11(8). |
| MLA | Sun, Changfeng,et al."Climate Response of Tree Radial Growth at Different Timescales in the Qinling Mountains".PLOS ONE 11.8(2016). |
入库方式： OAI收割
来源：地球环境研究所
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