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   内孤立子 在 海洋学 分类中 的翻译结果: 查询用时:1.243秒
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内孤立子
相关语句
  internal soliton
    Energy Dissipation and Velocity Distribution of Internal Soliton Encountering Submerged Triangular Obstacle
    内孤立子遇海脊障碍物的能量消散和速度分布
短句来源
  internal soliton
    Energy Dissipation and Velocity Distribution of Internal Soliton Encountering Submerged Triangular Obstacle
    内孤立子遇海脊障碍物的能量消散和速度分布
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  “内孤立子”译为未确定词的双语例句
    From the numerical results, it is shown that the initial internal solitary wave and the measured internal solitary all can fission when they pass through the continental slope.
    数值结果表明,深水区的初始内孤立波和实测的内孤立波(内潮)在通过陆坡区时都会产生分裂,并在陆架上(浅水区)生成一内孤立子波列。
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  internal soliton
Damping of internal soliton modes in media with quadratic nonlinearity
      
Internal soliton modes and the rate of their radiative damping as a function of detuning from the phase-matching condition and the nonlinear shift of phase velocity for different soliton dimensions (d=1, 2, 3) are found.
      
An estimation of internal soliton forces on a pile in the ocean
      
Internal soliton forces on oil-platform piles in the ocean are estimated with the Morison Formula.
      
Different from surface wave forces, which change only in magnitude along a pile, internal soliton forces can be distributed over the entire pile in the water and they change not only in magnitude but also in direction with depth.
      
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  internal soliton
Damping of internal soliton modes in media with quadratic nonlinearity
      
Internal soliton modes and the rate of their radiative damping as a function of detuning from the phase-matching condition and the nonlinear shift of phase velocity for different soliton dimensions (d=1, 2, 3) are found.
      
An estimation of internal soliton forces on a pile in the ocean
      
Internal soliton forces on oil-platform piles in the ocean are estimated with the Morison Formula.
      
Different from surface wave forces, which change only in magnitude along a pile, internal soliton forces can be distributed over the entire pile in the water and they change not only in magnitude but also in direction with depth.
      
更多          


A ray-type 2D-KdV equation for studying the fission of internal waves is derived in the present paper. By using a reduced equation resulted from the 2D-KdV equation, a numerical calculation on the fission of soliton-type internal wave and a measured internal solitary wave (or internal tide) is carried out at the laboratory scale. From the numerical results, it is shown that the initial internal solitary wave and the measured internal solitary all can fission when they pass through the continental slope. It is...

A ray-type 2D-KdV equation for studying the fission of internal waves is derived in the present paper. By using a reduced equation resulted from the 2D-KdV equation, a numerical calculation on the fission of soliton-type internal wave and a measured internal solitary wave (or internal tide) is carried out at the laboratory scale. From the numerical results, it is shown that the initial internal solitary wave and the measured internal solitary all can fission when they pass through the continental slope. It is concluded that the fission of the internal tides on the slope is one of the dominant generating mechanisms of internal soliton packets (or wave train) on the shelf under real ocean conditions.

本文导得了1个研究内波分裂的射线型二维KdV方程。利用这一方程的一维退化方程进行了实验室尺度下孤立子型内波分裂的数值研究。数值结果表明,深水区的初始内孤立波和实测的内孤立波(内潮)在通过陆坡区时都会产生分裂,并在陆架上(浅水区)生成一内孤立子波列。这表明在实际海洋条件下,深海区内潮的分裂是陆架上海洋内孤立子波包(或波列)生成的主要机制之一。

 
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