A correlation between southern and northern hemispheres during the last 0.6Ma
文献类型:期刊论文
作者 | Liu, DS; An, ZS; Chen, MY; Sun, DH |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
![]() |
出版日期 | 1996-04 |
卷号 | 39期号:2页码:113-120 |
关键词 | change of climate type at 0.6Ma BP Australia high and East Asia monsoon Mongolia high Australian summer monsoon |
文献子类 | Article |
英文摘要 | A comparison of climate records between Chinese Loess Plateau which shows a strengthening of summer monsoon in the last 0.6 Ma and a strengthening of Asia summer monsoon during 35-25 and 4-2.5 ka B.P. intervals, and the Australian records which show a strengthening of aridity or desertification suggest that the Australian high leading to the desertification strengthened the Asia summer monsoon in the past through the cross-equator circulation. The synchronous variation in the Holocene Optimum as indicated by Asia and Australia climate records, on the other hand, suggests that the cross-equator East Asia winter monsoon circulation related to the Mongolia high might have influenced the Australia summer monsoon. The interaction of the monsoon climate between southern and northern hemispheres through cross-equator circulation probably started to be obvious since 0.6 Ma B. P. |
学科主题 | Geology |
WOS研究方向 | Geosciences, Multidisciplinary |
语种 | 英语 |
WOS记录号 | WOS:A1996WA99900001 |
出版者 | SCIENCE CHINA PRESS |
源URL | [http://ir.ieecas.cn/handle/361006/12103] ![]() |
专题 | 黄土与第四纪地质国家重点实验室(1985-2004) |
推荐引用方式 GB/T 7714 | Liu, DS,An, ZS,Chen, MY,et al. A correlation between southern and northern hemispheres during the last 0.6Ma[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,1996,39(2):113-120. |
APA | Liu, DS,An, ZS,Chen, MY,&Sun, DH.(1996).A correlation between southern and northern hemispheres during the last 0.6Ma.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,39(2),113-120. |
MLA | Liu, DS,et al."A correlation between southern and northern hemispheres during the last 0.6Ma".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 39.2(1996):113-120. |
入库方式: OAI收割
来源:地球环境研究所
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。