Quantitative recuperation of climatic sequences for the last 200 years in Xingcuo Lake, eastern Tibetan Plateau
文献类型：期刊论文
| 作者 | Wu, JL; Schleser, GH; Wang, SM; Lucke, A; Li, SJ; Xia, WL; Shi, YF |
| 刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
 |
| 出版日期 | 2002 |
| 卷号 | 45期号:9页码:832-841 |
| 关键词 | Tibetan Plateau trace element stable isotope climatic signal |
| ISSN号 | 1006-9313 |
| 英文摘要 | The functional relation between the delta(18)O values in the shell of gastropod Gyraulus sibirica and the air temperature in the warm half-yearly period, and that between Sr/Ca ratio and the precipitation in the warm half-yearly period were established by calibrating the delta(18)O and delta(13)C values, Sr/Ca ratio and Mg/Ca ratio in the shell Gyraulus sibirica, as well as the total organic carbon (TOC) and its delta(13)C values in the Xingcuo Lake sediment in the eastern Tibetan Plateau. The sequences of air temperature and precipitation in the last 200 years in the region were quantitatively recuperated on this basis. The results showed the following: (i) There was a negative correlativity between Sr/Ca ratio and the precipitation in the warm half-yearly period, its correlation coefficient was 0.86. (ii) There was an obviously positive correlativity between index delta(18)O and the running average temperature in the warm half-yearly period, its correlation coefficient was 0.89. (iii) Evolution of the air temperature and the precipitation in the last 200 years can be divided into three phases distinctly. The precipitation in the later mid-19th century was 220 mm higher than that today; the air temperature in the warm half-yearly period was 2degreesC lower than that of the present. The precipitation in the minimum air temperature period of the early 20th century was below that today by 60 mm, and the air temperature in the warm half-yearly period was 3.4degreesC lower than that today. (iv) An evidently warming and drying trend existed in the last five decades. |
| 公开日期 | 2012-03-02 |
| 源URL | [http://159.226.73.51/handle/332005/2407]  |
| 专题 | 南京地理与湖泊研究所_湖泊室 |
| 推荐引用方式 GB/T 7714 | Wu, JL,Schleser, GH,Wang, SM,et al. Quantitative recuperation of climatic sequences for the last 200 years in Xingcuo Lake, eastern Tibetan Plateau[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2002,45(9):832-841. |
| APA | Wu, JL.,Schleser, GH.,Wang, SM.,Lucke, A.,Li, SJ.,...&Shi, YF.(2002).Quantitative recuperation of climatic sequences for the last 200 years in Xingcuo Lake, eastern Tibetan Plateau.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,45(9),832-841. |
| MLA | Wu, JL,et al."Quantitative recuperation of climatic sequences for the last 200 years in Xingcuo Lake, eastern Tibetan Plateau".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 45.9(2002):832-841. |
入库方式： OAI收割
来源：南京地理与湖泊研究所
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。