Regional hydroclimate and precipitation delta O-18 revealed in tree-ring cellulose delta O-18 from different tree species in semi-arid Northern China | |
Li,Q (Li, Qiang)[1]; Nakatsuka,T (Nakatsuka, Takeshi)[1]; Kawamura,K (Kawamura, Kimitaka)[2]; Liu,Y (Liu, Yu)[3,4]; Song, HM (Song, Huiming)[3] | |
2011-03-07 | |
发表期刊 | CHEMICAL GEOLOGY |
卷号 | 282期号:1-2页码:19-28 |
文章类型 | 期刊论文 |
摘要 | Oxygen isotopic ratios (delta(18)O) of tree-ring cellulose, grown from 1954 to 2003 in semi-arid Northern China demonstrate a common inter-annual variability, despite coming from three different species in two distinct growth environments (an alpine meadow and a rocky ridge). The variability was significantly negative correlated with precipitation and relative humidity during the growing season. This suggests that the past summer hydroclimate can be inferred from tree-ring cellulose delta(18)O from various kinds of trees growing in semi-arid Northern China. In addition, we evaluated past changes in delta(18)O of precipitation from the tree-ring cellulose delta(18)O and relative humidity using the mechanistic model for tree-ring cellulose delta(18)O in Roden et al. (2000). By fixing the species-dependent exchange rate of oxygen between carbohydrate and xylem water for Larix principis-rupprechtii and Picea koraiensis, we could also reconstruct the variations in precipitation delta(18)O from the different tree species, which are similar to the observed delta(18)O of precipitation during 1985-2002. Although the reconstructed delta(18)O of precipitation does not have any significant relation to local temperature or precipitation during 1954-2003, its long-term variation pattern is similar to that of the Asian summer monsoon indices and delta(18)O of stalagmite in the Heshang cave (30 degrees 27'N, 110 degrees 25'E; Fig. 1), suggesting that delta(18)O of precipitation is not controlled by local meteorology but is influenced by large-scale atmospheric circulation. |
关键词 | Tree-ring cellulose δ18O Hydroclimate δ18O of precipitation The Asian monsoon Northern China |
DOI | 10.1016/j.chemgeo.2011.01.004 |
收录类别 | SCI |
语种 | 英语 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ieecas.cn/handle/361006/10332 |
专题 | 现代环境研究室 |
通讯作者 | Li,Q (Li, Qiang)[1] |
作者单位 | 1.Graduate School of Environment Studies, Nagoya University, Nagoya 464-8601, Japan; 2.Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan; 3.Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China; 4.School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an 710049, China |
推荐引用方式 GB/T 7714 | Li,Q ,Nakatsuka,T ,Kawamura,K ,et al. Regional hydroclimate and precipitation delta O-18 revealed in tree-ring cellulose delta O-18 from different tree species in semi-arid Northern China[J]. CHEMICAL GEOLOGY,2011,282(1-2):19-28. |
APA | Li,Q ,Nakatsuka,T ,Kawamura,K ,Liu,Y ,&Song, HM .(2011).Regional hydroclimate and precipitation delta O-18 revealed in tree-ring cellulose delta O-18 from different tree species in semi-arid Northern China.CHEMICAL GEOLOGY,282(1-2),19-28. |
MLA | Li,Q ,et al."Regional hydroclimate and precipitation delta O-18 revealed in tree-ring cellulose delta O-18 from different tree species in semi-arid Northern China".CHEMICAL GEOLOGY 282.1-2(2011):19-28. |
条目包含的文件 | ||||||
文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
Regional hydroclimat(2466KB) | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | 请求全文 |
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。
修改评论