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DOI | 10.1029/2007GL030853 |
Dust storm activity over the Tibetan Plateau recorded by a shallow ice core from the north slope of Mt. Qomolangma (Everest), Tibet-Himal region | |
Xu, Jianzhong; Hou, Shugui; Qin, Dahe; Kang, Shichang; Ren, Jiawen; Ming, Jing | |
发表日期 | 2007 |
ISSN | 0094-8276 |
EISSN | 1944-8007 |
卷号 | 34期号:17 |
英文摘要 | Based on a 39.8 m ice core drilled at the East Rongbuk Glacier (27 degrees 590N, 86 degrees 55'E 6518 m a.s.l,), north slope of Mt. Qomolangma (Everest), central Himalaya, the changes of dust storm over the Tibetan Plateau (TP) recorded by insoluble particle and its possible connection with the winter (JFM) North Atlantic Oscillation (NAO) are investigated. The results show that the level of dust storm activity exhibits a significant decreasing trend during the past similar to 50 years. This may be attributed, at least partly, to a decrease in wind speed over the TP and its surrounding regions. The normalized time series of the winter NAO index shows a significant inverse correlation with the mass concentration of insoluble particle implying a possible connection between the winter NAO and the dust storm activity over the TP. |
关键词 | DESERT DUSTMONSOONCHINAPRECIPITATIONOSCILLATIONDEPOSITIONCLIMATETRENDSASIA |
学科领域 | Geology |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000249518300008 |
来源期刊 | GEOPHYSICAL RESEARCH LETTERS |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/111480 |
推荐引用方式 GB/T 7714 | Xu, Jianzhong,Hou, Shugui,Qin, Dahe,et al. Dust storm activity over the Tibetan Plateau recorded by a shallow ice core from the north slope of Mt. Qomolangma (Everest), Tibet-Himal region[J]. 中国科学院青藏高原研究所,2007,34(17). |
APA | Xu, Jianzhong,Hou, Shugui,Qin, Dahe,Kang, Shichang,Ren, Jiawen,&Ming, Jing.(2007).Dust storm activity over the Tibetan Plateau recorded by a shallow ice core from the north slope of Mt. Qomolangma (Everest), Tibet-Himal region.GEOPHYSICAL RESEARCH LETTERS,34(17). |
MLA | Xu, Jianzhong,et al."Dust storm activity over the Tibetan Plateau recorded by a shallow ice core from the north slope of Mt. Qomolangma (Everest), Tibet-Himal region".GEOPHYSICAL RESEARCH LETTERS 34.17(2007). |
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