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DOI | 10.1016/j.gloplacha.2015.03.008 |
Magnetic variations in surface soils in the NE Tibetan Plateau indicating the climatic boundary between the Westerly and East Asian summer monsoon regimes in NW China | |
Zan, Jinbo; Fang, Xiaomin; Yan, Maodu; Zhang, Weilin; Zhang, Zhiguo | |
通讯作者 | Zan, JB (通讯作者) |
发表日期 | 2015 |
ISSN | 0921-8181 |
EISSN | 1872-6364 |
起始页码 | 1 |
结束页码 | 6 |
卷号 | 130 |
英文摘要 | Two atmospheric circulation systems, i.e., the mid-latitude Westerlies and the East Asian summer monsoon (EASM), dominate climate change in the NE Tibetan Plateau. However, controversy remains with regard to the climatic boundary between these westerly and monsoon regimes. In this paper, detailed rock magnetic and geochemical Rb/Sr analyses for a larger number of surface soils from a wide area in the NE Tibetan Plateau are presented. They show that surface soils in this region evince relatively significant regional variations in magnetic properties and geochemical characteristics. The magnetic parameters chi(fd), chi(ARM) and geochemical Rb/Sr ratios exhibit higher values in EASM-controlled (humid) areas, and lower values in Westerlies-influenced (arid) areas. These characteristics indicate that such variations in chi(fd), chi(ARM) and Rb/Sr ratios can be regarded as effective indicators of the degree of pedogenesis and weathering in the NE Tibetan Plateau. Our results also demonstrate that the climatic boundary between the westerly and monsoon regimes approximately overlaps with the boundary of highland meadow and temperate steppe desert/desert in NW China. (C) 2015 Elsevier B.V. All rights reserved. |
关键词 | LOESS-PALEOSOL SEQUENCESGRAIN-SIZESUSCEPTIBILITYPEDOGENESISPROFILESBASINLAKE |
英文关键词 | Surface soils; Environmental magnetism; Rb/Sr ratio; Tibetan Plateau; Climatic boundary |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000356206800001 |
来源期刊 | GLOBAL AND PLANETARY CHANGE
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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/258418 |
推荐引用方式 GB/T 7714 | Zan, Jinbo,Fang, Xiaomin,Yan, Maodu,et al. Magnetic variations in surface soils in the NE Tibetan Plateau indicating the climatic boundary between the Westerly and East Asian summer monsoon regimes in NW China[J]. 中国科学院青藏高原研究所,2015,130. |
APA | Zan, Jinbo,Fang, Xiaomin,Yan, Maodu,Zhang, Weilin,&Zhang, Zhiguo.(2015).Magnetic variations in surface soils in the NE Tibetan Plateau indicating the climatic boundary between the Westerly and East Asian summer monsoon regimes in NW China.GLOBAL AND PLANETARY CHANGE,130. |
MLA | Zan, Jinbo,et al."Magnetic variations in surface soils in the NE Tibetan Plateau indicating the climatic boundary between the Westerly and East Asian summer monsoon regimes in NW China".GLOBAL AND PLANETARY CHANGE 130(2015). |
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