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| DOI | 10.1360/982005-237 |
| Decrease trend of dust event frequency over the past 200 years recorded in the Malan ice core from the northern Tibetan Plateau | |
| Wang, NL | |
| 发表日期 | 2005 |
| ISSN | 1001-6538 |
| EISSN | 1861-9541 |
| 起始页码 | 2866 |
| 结束页码 | 2871 |
| 卷号 | 50期号:24 |
| 英文摘要 | By analyses of the dust layers in the Malan ice core from the northern Tibetan Plateau, it was found that dirty ratio in this core might be a good proxy for dust event frequency. The variations in the dirty ratio displayed a decrease trend over the past 200 years, which implies that dust events became less frequent during the study period. The decrease trend in the variations in dust event frequency might be caused mostly by the natural processes, including increasing precipitation and weakening westerly which might be related with global warming. Furthermore, significant negative correlation was found between the dirty ratio and 45180 in the Malan ice core. This is highly important for studying the effect of atmospheric dust on climate change. |
| 关键词 | MINERAL DUSTAFRICAN DUSTAEROSOLCLIMATEATMOSPHERETRANSPORTDESERTIFICATIONABSORPTIONSATELLITESTORMS |
| 英文关键词 | dust event; climate change; Malan ice core; Tibetan Plateau |
| 语种 | 英语 |
| WOS研究方向 | Science & Technology - Other Topics |
| WOS类目 | Multidisciplinary Sciences |
| WOS记录号 | WOS:000235457500014 |
| 来源期刊 | CHINESE SCIENCE BULLETIN
 |
| 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/257364 |
| 推荐引用方式 GB/T 7714 | Wang, NL. Decrease trend of dust event frequency over the past 200 years recorded in the Malan ice core from the northern Tibetan Plateau[J]. 中国科学院青藏高原研究所,2005,50(24). |
| APA | Wang, NL.(2005).Decrease trend of dust event frequency over the past 200 years recorded in the Malan ice core from the northern Tibetan Plateau.CHINESE SCIENCE BULLETIN,50(24). |
| MLA | Wang, NL."Decrease trend of dust event frequency over the past 200 years recorded in the Malan ice core from the northern Tibetan Plateau".CHINESE SCIENCE BULLETIN 50.24(2005). |
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