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DOI | 10.1360/03wd0417 |
Relationship between calcium and atmospheric dust recorded in Guliya ice core | |
Yao, TD![]() | |
发表日期 | 2004 |
ISSN | 1001-6538 |
EISSN | 1861-9541 |
起始页码 | 706 |
结束页码 | 710 |
卷号 | 49期号:7页码:706-710 |
英文摘要 | By the analyses of Guliya ice core on the Tibetan Plateau, it was found that the calcium (Ca2+) originated from the terrestrial source is the main cation of soluble aerosol and a good proxy of the atmospheric component and environment in the mountain ice core located in the mid-low latitude arid regions. Evident variation of Ca2+ concentration has been found in the Guliya ice core since the Last Interglaciation with two relatively strong increase periods and two weak increase periods. These variations are generally related to climatic changes: high Ca2+ concentration periods coincide with cold periods and low Ca2+ concentration periods coincide with warm periods. However, Ca2+ concentration does not always decrease (increase) with climate warming (cooling). The magnitude and phase of Ca2+ concentration does not always match temperature either. The changes of atmospheric circulation, land surface condition and atmospheric humidity might be important factors which influence Ca2+ concentration besides temperature. |
关键词 | GREENLAND ICECLIMATEDEPOSITIONPLATEAUVOSTOKCHINACYCLESEAAGE |
英文关键词 | Guliya ice core; Ca2+; dust |
语种 | 英语 |
WOS研究方向 | Science & Technology - Other Topics |
WOS类目 | Multidisciplinary Sciences |
WOS记录号 | WOS:000222338600012 |
来源期刊 | CHINESE SCIENCE BULLETIN
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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/456 |
推荐引用方式 GB/T 7714 | Yao, TD,Wu, GJ,Pu, JC,et al. Relationship between calcium and atmospheric dust recorded in Guliya ice core[J]. 中国科学院青藏高原研究所,2004,49(7):706-710. |
APA | Yao, TD,Wu, GJ,Pu, JC,Jiao, KQ,&Huang, CL.(2004).Relationship between calcium and atmospheric dust recorded in Guliya ice core.CHINESE SCIENCE BULLETIN,49(7),706-710. |
MLA | Yao, TD,et al."Relationship between calcium and atmospheric dust recorded in Guliya ice core".CHINESE SCIENCE BULLETIN 49.7(2004):706-710. |
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