内波传播方向以西向为主。
这些波浪，内波，可能会有几万米长，持续几个小时。
These waves, internal waves, can be tens of kilometers long and can last several hours.
海洋内波垂向结构的求解有不同的数学方法。
There are several different mathematical methods used in solving the vertical structure of ocean internal waves.
对流强迫重力内波的生成机制和向平流层的传播。
Generation Mechanisms of Convectively Forced Internal Gravity Waves and Their Propagation to the Stratosphere.
这张图片显示了印度洋安达曼群岛附近的内波和表面流。
This image shows both internal waves and surface waves on the Indian Ocean near the Andaman Islands.
将基于两层流假定下的两种水面条件内波解进行了对比。
The paper studies the character of dispersion relations of two internal wave solutions with different water surface condition in two-layer fluid.
内波、内潮汐沉积是近10多年来沉积学研究的一个新领域。
Internal wave and internal tide deposits are a new field of sedimentological research in the latest 10 years.
内波不仅可以沿着水平方向传播，而且还具有垂向传播的特性。
The internal waves can propagate along the level direction and the perpendicularity one.
明确指向沉积构造的形成机理对于内波沉积的识别具有重要意义。
The generation mechanism of orientating sedimentary structure is very important to the recognition of the internal-waves sediments.
本文给出了由运动物体所生成内波的基本方程组和对应的谱方程组。
A basic equation of internal waves generated by moving body and its corresponding spectrum equation are presented in this paper.
运输问题，河流量问题，内波问题，机械振动和其他物理学问题的应用。
Applications to traffic problems, flows in rivers, internal waves, mechanical vibrations and other problems in the physical world.
在一定条件下，遥感图像上可以观测到舰船的尾迹或自然界的内波现象。
In some condition the wake of ship or the natural interwave can be observed in remote sensing imagery.
在等深流与上覆低密度水体之间的界面上具备产生大规模界面内波的条件；
The contour currents colliding with the overlapped low density normal seawater can create internal waves of large scale at the interface of the thermohaline.
实验中的密度分层采用典型跃层型剖面，而内波是由自行研制的造波机生成。
In this experiment, typical pycnocline-type profiles are employed, and the internal waves are generated by a wave maker designed by the authors.
在综合分析的基础上，进一步建立了该区水道型和非水道型内波内潮汐沉积模式。
Finally, the inter wave and inter tide sedimentary model of channels and non channels has been established on the basis of comprehensive analysis.
海洋上大致水平方向的小波纹是表面流，图片右侧内波在海洋上划出了长长的对角线。
The tiny wrinkles running roughly horizontally across the ocean are surface waves. Internal waves paint long diagonal lines across the ocean on the right side of the image.
表面惯性重力波和惯性重力内波的相速公式都是这个更普遍的频率方程的特殊情况。
The well-known phase speed formulas of surface inertial gravity wave and internal shear inertial gravity wave are the special cases of this frequency equation.
本文首先从地球流体力学基本方程出发，通过一些基本假设，推导出海洋内波控制方程。
In the thesis, we firstly derive control equations of oceanic internal wave by basic hypothesis which is based on equation of Geophysical Fluid Mechanics.
在这类强迫方程的源项中包含了10类内波谱，这些谱最终均可利用内波的振幅谱表示。
There exist 10 spectra in the source terms of the nonlinear spectra equation, and all the unknown spectrum can be denoted in terms of the amplitude spectrum.
本文利用CTD数据及线性内波模型，并结合内波的GM谱特性，求得线性内波的垂直位移。
In this paper, associated with the GM spectrum, the vertical displacements of linear internal waves were obtained by using CTD data and linear internal wave modeling.
孤立子内波在传播过程中所产生的突发性强流对海洋工程、石油钻井平台等会造成严重的破坏。
The sudden strong current induced by internal soliton during its propagation can cause severe threat to the ocean engineering and oil drilling platform etc.
海洋内孤立波是一种携带巨大能量的特殊内波，它能够在海洋中长距离传播而保持波形基本不变。
Internal solitary waves are a kind of special internal waves, which could bring enormous energy and propagate long distance in the ocean with its wave form basically unchanged.
出现内波是因为海洋是分层的，深层水更凉，密度高而且含盐量高，浅层水更暖和，密度小而且更淡。
Internal waves happen because the ocean is layered. Deep water is cold, dense, and salty, while shallower water is warmer, lighter, and fresher.
本研究将“边缘层模型”应用于两层流体系统中弱非线性内波在台阶地形上的反射和透射问题的研究。
The edge-layer theory is applied to study the refection and transmission of the weakly nonlinear internal wave over a step in a two-layer fluid system.
这可能是地层中深水复合流沉积构造的首次发现，同时也是内波与浊流形成的复合流沉积的首次发现。
This perhaps is the first discovery of deep-water sedimentary structure of combined-flow origin as well as the combined-flow deposition produced by internal wave and turbidity current.
目前SAR经常用于内波的研究，但是SAR也存在着卫星重访周期长、数据费用高、图像噪声较大等的不足。
SAR imagery are usually available at the present research, however SAR are deficient for the long revisit period, high expense and strong noise.
本文应用WKB方法研究了在弱非均匀层结大气中，当基本气流具有弱垂直切变时，重力惯性内波的稳定性问题。
This paper discusses the stability of internal inertial gravity wave in the heterogeneous stratified atmosphere when basic flow appears to be weak vertical shear by the WKB method.
本文应用WKB方法研究了在弱非均匀层结大气中，当基本气流具有弱垂直切变时，重力惯性内波的稳定性问题。
This paper discusses the stability of internal inertial gravity wave in the heterogeneous stratified atmosphere when basic flow appears to be weak vertical shear by the WKB method.
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