Influence of the earth rotation on the interfacial wave solutions and wave-induced tangential stress in a two-layer fluid system
文献类型:期刊论文
作者 | Song Jinbao1,2; Liu Yongjun1,2,3 |
刊名 | ACTA OCEANOLOGICA SINICA
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出版日期 | 2009 |
卷号 | 28期号:2页码:115-120 |
关键词 | Two-layer Fluid Interfacial Waves Wave-induced Tangential Stress Earth Rotation |
ISSN号 | 0253-505X |
文献子类 | Article |
英文摘要 | Interfacial waves and wave-induced tangential stress are studied for geostrophic small amplitude waves of two-layer fluid with a top free surface and a flat bottom. The solutions were deduced from the general form of linear fluid dynamic equations of two-layer fluid under the f-plane approximation, and wave-induced tangential stress were estimated based on the solutions obtained. As expected; the solutions derived from the present work include as special cases those obtained by Sun et al. (2004. Science in China, Set. D, 47(12): 1147-1154) for geostrophic small amplitude surface wave solutions and wave-induced tangential stress if tire density of the upper layer is much smaller than that of the lower layer. The results show that the interface and the surface will oscillate synchronously, and the influence of the earth's rotation both on the surface wave solutions and the interfacial wave solutions should be considered.; Interfacial waves and wave-induced tangential stress are studied for geostrophic small amplitude waves of two-layer fluid with a top free surface and a flat bottom. The solutions were deduced from the general form of linear fluid dynamic equations of two-layer fluid under the f-plane approximation, and wave-induced tangential stress were estimated based on the solutions obtained. As expected; the solutions derived from the present work include as special cases those obtained by Sun et al. (2004. Science in China, Set. D, 47(12): 1147-1154) for geostrophic small amplitude surface wave solutions and wave-induced tangential stress if tire density of the upper layer is much smaller than that of the lower layer. The results show that the interface and the surface will oscillate synchronously, and the influence of the earth's rotation both on the surface wave solutions and the interfacial wave solutions should be considered. |
学科主题 | Oceanography |
语种 | 英语 |
WOS记录号 | WOS:000266647100012 |
公开日期 | 2010-12-22 |
源URL | [http://ir.qdio.ac.cn/handle/337002/2395] ![]() |
专题 | 海洋研究所_海洋环流与波动重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, KLOCAW, Qingdao 266071, Peoples R China 3.Chinese Acad Sci, Grad Univ, Beijing 100039, Peoples R China |
推荐引用方式 GB/T 7714 | Song Jinbao,Liu Yongjun. Influence of the earth rotation on the interfacial wave solutions and wave-induced tangential stress in a two-layer fluid system[J]. ACTA OCEANOLOGICA SINICA,2009,28(2):115-120. |
APA | Song Jinbao,&Liu Yongjun.(2009).Influence of the earth rotation on the interfacial wave solutions and wave-induced tangential stress in a two-layer fluid system.ACTA OCEANOLOGICA SINICA,28(2),115-120. |
MLA | Song Jinbao,et al."Influence of the earth rotation on the interfacial wave solutions and wave-induced tangential stress in a two-layer fluid system".ACTA OCEANOLOGICA SINICA 28.2(2009):115-120. |
入库方式: OAI收割
来源:海洋研究所
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