The change of characteristics of tidal wave in the Changjiang River mouth area since the post-glacial transgression maximum | |
Zhu, YR | |
2001-08-01 | |
发表期刊 | SCIENCE IN CHINA SERIES B-CHEMISTRY |
ISSN | 1006-9291 |
卷号 | 44页码:107-111 |
文章类型 | Article |
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. |
关键词 | Post-glacial Transgression Maximum Changjiang River Mouth Tidal Wave Characteristics |
学科领域 | Chemistry, Multidisciplinary |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000171498900014 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/3828 |
专题 | 海洋地质与环境重点实验室 |
作者单位 | 1.Shanghai Jiao Tong Univ, Sch Environm Sci & Engn, Shanghai 200240, Peoples R China 2.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, 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. |
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