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solitary
相关语句
  孤立
    NONLINEAR ROSSBY WAVE AND SOLITARY WAVE INFLUENCED BY THE HEAT SOURCE IN THE BAROTROPIC NONDIVERGENT ATMOSPHERE
    特定外源下的非线性Rossby椭圆余弦波和孤立
短句来源
    THE EFFECTS OF OROGRAPHY ON THE SOLITARY ROSSBY WAVES IN A BAROTROPIC ATMOSPHERE
    大地形与正压Rossby孤立
短句来源
    LARGE OROGRAPHY AND BAROTROPIC SOLITARY ROSSBY WAVES——WEAK QUADRIC SHEARING BASIC FLOW
    大地形与正压Rossby孤立波——弱二次切变基本气流
短句来源
    Baroclinic Solitary Rossby Waves in a N-Level Model
    N层模式大气中的斜压孤立Rossby波
短句来源
    ALGEBRAIC SOLITARY ROSSBY WAVE IN THE ATMOSPHERE
    正压大气中的代数Rossby孤立
短句来源
更多       
  
    SOLITARY ROSSBY WAVES OF TROPICAL ATMOSPHERIC MOTION
    热带大气运动的Rossby
短句来源
    INFLUENCES OF INTERACTION OF EXTERNAL SOURCE WITH SOLITARY WAVE ON BLOCKING
    外源与波的相互作用对阻塞形成的影响
短句来源
    A TYPE OF SINGULAR SOLITARY WAVE AND ITS APLLICATION OF STRUCTURE ANALYSIS OF THE TIBETAN PLATAU VORTEX
    一类奇异波解及其在高原低涡结构分析中的应用
短句来源
    INFLUENCES OF DISSIPATION ON INTERACTION OF SOLITARY WAVE WITH LOCALIZED TOPOGRAPHY
    耗散对波与局地地形相互作用的影响(英文)
短句来源
    This paper theoritically proves that the formation and the evolution of squall lines in the baroclinic, non-static atmosphere, as in the barotropic atmosphere, may be referred to a kind of atmospheric solitary wave described by the K-dV equation.
    本文从理论上证明斜压非静力平衡大气中飑线的形成与演变和正压大气中一样可以归结为一类由K-dV方程所描述的大气波.
短句来源
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  “solitary”译为未确定词的双语例句
    SOLITARY GRAVITY WAVE CHARACTERISTICS OF VERTICAL CIRCULATION ADJACENT TO FRONTS
    锋面附近垂直环流的重力波特征
短句来源
    THE ENVELOPE SOLITARY WAVE SOLUTION OF INERTIA-GRAVITATION WAVE IN THE ATMOSPHERE
    大气中惯性重力内波的调制
短句来源
    In this paper, the WKB method is used to obtain the nonlineas schrodinger equation satisfied by nonlinear inertia-gravitatrnal wave in the atmosphere, It is found that the nonlineas schiodinges equation has envelope solitary wave solution.
    本文用WKB方法讨论大气中惯性重力内波的调制问题,得到了Schrodinger方程及其包络孤立子解。
短句来源
    To find the solution of the single varible equation whichcan be reduced to the KdV equation, the nonlinear cnoidal wave and solitary wave areobtained.
    这是与KdV方程相应的非线性常微分方程,可得到椭圆余弦波或弧立波。
短句来源
    It gets the Sine Gordon equation and its solitary wave solution.
    在引入时空缓变量后,导出Sine-Gordon方程,并求得了孤立子解
短句来源
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  solitary
This paper considers the generalized KdV equation with or without natural boundary conditions and provides a parameter region for solitons and solitary waves, and also modifies a result of Zabusky's.
      
The exact solutions and solitary solutions of NLPDE are obtained.
      
With modulus m → 1 or m → 0, these solutions degenerate into corresponding solitary wave solutions, shock wave solutions and trigonometric function solutions.
      
As is well known, Korteweg-de Vries equation is a typical one which has planar solitary wave.
      
By considering higher order transverse disturbance to planar solitary waves, we study a Kadomtsev-Petviashvili (KP) equation and find some interesting results.
      
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In this paper, from the system of equations describing a barotropie atmosphere, using the method of Taylor expansion for the nonlinear terms, the periodic solutions of the nonlinear surface inertio-gravitational waves and Rossby waves have been obtained.The finite-amplitude nonlinear surface inertio-gravitational waves and Rossby waves with horizontal divergence satisfy the KdV equation. Its solution is a cnoidal wave which consists of linear waves and forms solitary waves under certain conditions. For...

In this paper, from the system of equations describing a barotropie atmosphere, using the method of Taylor expansion for the nonlinear terms, the periodic solutions of the nonlinear surface inertio-gravitational waves and Rossby waves have been obtained.The finite-amplitude nonlinear surface inertio-gravitational waves and Rossby waves with horizontal divergence satisfy the KdV equation. Its solution is a cnoidal wave which consists of linear waves and forms solitary waves under certain conditions. For the finite-amplitude Rossby waves with horizontal divergence, we find the new dispersive relation which contains the amplitude parameter. In case of small amplitude it is reduced to the Yeh formula. It is shown that the larger the amplitude and width, the faster the finite-amplitude surface inertio-gravitational waves and the slower the finite-amplitude Rossby waves with horizontal divergence propagate. The blocking or cut-off system in which the amplitude and width are large may be considered as Rossby solitary wave.

本文从非线性大气运动正压模式方程组出发,用我们所设计的将非线性项在平衡点附近作Taylor展开的方法,求得了非线性有限振幅的惯性-重力外波和有辐散的Rossby波,均满足著名的KdV方程,它的解为椭圆余弦波,它包含线性波动,在一定的条件下形成孤立波。对有限振幅的但有辐散的Rossby波,它包含线性的有辐散的Rossby波(即叶笃正波),而且建立了包含叶笃正公式在内的新的色散关系,它含有振幅因子。分析表明:对有限振幅的惯性-重力外波,振幅大、宽度大的波传播越快,但对有限振幅的有辐散的Rossby波,振幅大、宽度大的波传播越慢,阻塞、切断系统可能属于Rossby孤立波。

This paper theoritically proves that the formation and the evolution of squall lines in the baroclinic, non-static atmosphere, as in the barotropic atmosphere, may be referred to a kind of atmospheric solitary wave described by the K-dV equation. The baroclinity and the non-static state of the atmosphere as well as the vertical shear of basic flow have influences on the characteristics and the structure of the solitary wave. When an initial disturbance with limited width occurs along the lower jet,...

This paper theoritically proves that the formation and the evolution of squall lines in the baroclinic, non-static atmosphere, as in the barotropic atmosphere, may be referred to a kind of atmospheric solitary wave described by the K-dV equation. The baroclinity and the non-static state of the atmosphere as well as the vertical shear of basic flow have influences on the characteristics and the structure of the solitary wave. When an initial disturbance with limited width occurs along the lower jet, this kind of solitary wave may be excited. If the strength and the width of the disturbance reach definite values, a train of solitary waves lined up forms. This is just the arrangement phenomenon of squall lines or thunderstorm complex observed in the atmosphere.

本文从理论上证明斜压非静力平衡大气中飑线的形成与演变和正压大气中一样可以归结为一类由K-dV方程所描述的大气孤波.讨论了在具有垂直切变的基本气流中这类孤波的结构特征,并与观测事实作了对比.当沿着低空急流出现有限宽度的初始扰动时,这种孤波可以被激发出来.当扰动的强度与宽度达到一定值时,还将形成一种孤波队列.这正是大气中所观测到的飑线或雷雨列队现象.

In this paper, starting from the primitive equations, the authors derive the K-dV equation which describes the solitary Rossby waves in the tropical atmosphere, and indicate that since these waves are ageostrophic, they differ from the quasi-geostrophic solitary Rossby waves studied by Redekopp etc. Owing to the non-linear action, these waves are also different from the linear waves of the tropical atmosphere. The authors believe that the persistency of some tropical atmospheric waves reflects the...

In this paper, starting from the primitive equations, the authors derive the K-dV equation which describes the solitary Rossby waves in the tropical atmosphere, and indicate that since these waves are ageostrophic, they differ from the quasi-geostrophic solitary Rossby waves studied by Redekopp etc. Owing to the non-linear action, these waves are also different from the linear waves of the tropical atmosphere. The authors believe that the persistency of some tropical atmospheric waves reflects the characteristic of the solitary waves that energy does not disperse.

广东热带海洋气象研究所

 
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