| GENERATION OF NONLINEAR INTERNAL WAVES ON CONTINENTAL SHELF |
| |
| 作者姓名： | Xu Zhao ting Yao Feng chao Wang Mei Physical Oceanography Laboratory and Institute of Physical Oceanography Ocean University of Qingdao China Key Laboratory of Marine Science and Numerical Modeling State Oceanic Administration Qingdao |
| |
| 作者单位： | Xu Zhao ting，Yao Feng chao，Wang Mei Physical Oceanography Laboratory and Institute of Physical Oceanography，Ocean University of Qingdao 266003，China Key Laboratory of Marine Science and Numerical Modeling，State Oceanic Administration，Qingdao 26 |
| |
| 基金项目： | theNaturalScienceFoundationofChina (grantNo:4 97762 84 ) |
| |
| 摘 要： | 1 . ＩＮＴＲＯＤＵＣＴＩＯＮＩｎｔｅｒｎａｌｔｉｄａｌｉｎｔｅｒａｃｔｉｏｎｗｉｔｈｂｏｔｔｏｍｆｅａｔｕｒｅｓａｐｐｅａｒｓｔｏｂｅｔｈｅｄｏｍｉｎａｎｔｍｅｃｈａｎｉｓｍｆｏｒｇｅｎｅｒａ ｔｉｏｎｏｆｔｈｅｃｏｈｅｒｅｎｔｏｃｅａｎｉｃｉｎｔｅｒｎａｌｗａｖｅｓｔｈａｔａｒｅｏｂｓｅｒｖａｂｌｅｗｉｔｈＳＡＲ ,ｃｌｏｓｅｒｔｏｓｈｏｒｅ ,ｒｉｖｅｒｉｎｅｏｒｇｌａｃｉａｌｉｎｔｒｕｓｉｏｎａｎｄｃｏｎｔｉｎｅｎｔａｌｂｒｅａｋｐｒｏｖｉｄｅｓｅｃ ｏｎｄａｒｙｇｅｎｅｒａｔｉｎｇｍｅｃｈａ…
|
GENERATION OF NONLINEAR INTERNAL WAVES ON CONTINENTAL SHELF |
| |
| Xu Zhao ting,Yao Feng chao,Wang Mei Physical Oceanography Laboratory and Institute of Physical Oceanography,Ocean University of Qingdao ,China Key Laboratory of Marine Science and Numerical Modeling,State Oceanic Administration,Qingdao .GENERATION OF NONLINEAR INTERNAL WAVES ON CONTINENTAL SHELF[J].Journal of Hydrodynamics,2001(3). |
| |
| Authors: | Xu Zhao ting Yao Feng chao Wang Mei Physical Oceanography Laboratory and Institute of Physical Oceanography Ocean University of Qingdao China Key Laboratory of Marine Science and Numerical Modeling State Oceanic Administration Qingdao |
| |
| Affiliation: | Xu Zhao ting,Yao Feng chao,Wang Mei Physical Oceanography Laboratory and Institute of Physical Oceanography,Ocean University of Qingdao 266003,China Key Laboratory of Marine Science and Numerical Modeling,State Oceanic Administration,Qingdao 26 |
| |
| Abstract: | A 2 D KdV equation is derived under condition of arbitrary continuous density profiles. A non fission version of initial internal solitary waves propagating onto the continental shelf is studied by means of the 2 D KdV equation. Under non Bohr and Sommerfeld's condition, numerical calculations are carried out based on the KdV equation. The results shows that the initial internal solitary waves in deep ocean break down into internal undular bores on the continental shelf. And the bores have a like soliton leading fronts and undular trails. |
| |
| Keywords: | KdV equation internal undular bore internal undular solitary wave internal solition |
| 本文献已被 CNKI 等数据库收录！ |
