The change of characteristics of tidal wave in the Changjiang River mouth area since the post-glacial transgression maximum
文献类型:期刊论文
作者 | Zhu, YR |
刊名 | SCIENCE IN CHINA SERIES B-CHEMISTRY
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出版日期 | 2001-08-01 |
卷号 | 44页码:107-111 |
关键词 | Post-glacial Transgression Maximum Changjiang River Mouth Tidal Wave Characteristics |
ISSN号 | 1006-9291 |
文献子类 | Article |
英文摘要 | During the period of the post-glacial transgression maximum (PGTM), there was a huge trumpet estuary in the modern Changjiang River Delta area. The location and the shape of the Paleo-Changjiang River Estuary (PCRE) were much different from those of the present Changjiang River Estuary. The study on the change of characteristics of tidal wave in the Changjiang River mouth area since the PGTM can help to understand better the dynamic development of the Changjiang River Delta. The course curves of tidal level and tidal current velocity during a single tidal cycle for 35 points are calculated, and characteristics of tidal waves in the PCRE and its adjacent area are compared with those of tidal waves in the modern Changjiang River mouth area. The results show that the tidal waves within the PCRE and in its adjacent area during the period of the PGTM belonged to standing wave or a mixture of standing wave and progressive wave. Since then, the tidal wave in the Changjiang River mouth become gradually to be progressive wave with the PCRE being filled and the Changjiang River mouth shifting southeastwards.; During the period of the post-glacial transgression maximum (PGTM), there was a huge trumpet estuary in the modern Changjiang River Delta area. The location and the shape of the Paleo-Changjiang River Estuary (PCRE) were much different from those of the present Changjiang River Estuary. The study on the change of characteristics of tidal wave in the Changjiang River mouth area since the PGTM can help to understand better the dynamic development of the Changjiang River Delta. The course curves of tidal level and tidal current velocity during a single tidal cycle for 35 points are calculated, and characteristics of tidal waves in the PCRE and its adjacent area are compared with those of tidal waves in the modern Changjiang River mouth area. The results show that the tidal waves within the PCRE and in its adjacent area during the period of the PGTM belonged to standing wave or a mixture of standing wave and progressive wave. Since then, the tidal wave in the Changjiang River mouth become gradually to be progressive wave with the PCRE being filled and the Changjiang River mouth shifting southeastwards. |
学科主题 | Chemistry, Multidisciplinary |
语种 | 英语 |
WOS记录号 | WOS:000171498900014 |
公开日期 | 2010-12-22 |
源URL | [http://ir.qdio.ac.cn/handle/337002/3829] ![]() |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Shanghai Jiao Tong Univ, Sch Environm Sci & Engn, Shanghai 200240, Peoples R China |
推荐引用方式 GB/T 7714 | Zhu, YR. The change of characteristics of tidal wave in the Changjiang River mouth area since the post-glacial transgression maximum[J]. SCIENCE IN CHINA SERIES B-CHEMISTRY,2001,44:107-111. |
APA | Zhu, YR.(2001).The change of characteristics of tidal wave in the Changjiang River mouth area since the post-glacial transgression maximum.SCIENCE IN CHINA SERIES B-CHEMISTRY,44,107-111. |
MLA | Zhu, YR."The change of characteristics of tidal wave in the Changjiang River mouth area since the post-glacial transgression maximum".SCIENCE IN CHINA SERIES B-CHEMISTRY 44(2001):107-111. |
入库方式: OAI收割
来源:海洋研究所
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