海水运动
- 网络seawater movement
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为了消除海水运动对需要保持稳定姿态物体的影响,设计了两轴稳定平台。
Seawater movement affects object which need keeping stable gesture . In order to remove this effect , two-axis stable platform is designed .
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另外作者还探讨了有关GIS与潮汐数值模拟系统及海水运动可视化系统的集成问题。
In this paper , the system integration of geographic information system , tide numerical simulation system and tide movement visualization system are discussed as an example for related studies .
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此外,理论表明,海水运动会产生感应电磁场。
In addition , the theory suggests that the seawater Games induction electromagnetic field .
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基于统计模型的海水运动仿真
Seawater Motion Simulation Based-on Statistic Model
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冰层下海水的运动常常会引起地表许多不同的变化。
The movement of the ocean water under the ice may often cause many different changes on the surface .
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海水垂直运动中的状态研究
The characters of vertical motion in the sea
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她唯一参与的是在光明会科学家触发地震后不可避免的起初的陆地和海水的运动。
Her only involvement was the unavoidable initial movements of land and water after Illuminati scientists triggered the quake .
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如何根据海水的运动现象和一些必要的外界条件将海水的涡黏性系数剖面反演出来,进而了解海洋内部运动信息是本论文的一个主要目标。
Accordingly , how to calculate and attain the profile of eddy viscosity parameter out of the phenomenon of ocean motions and some other necessary environment conditions is the main purpose of the thesis .
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地形Rossby波非线性相互作用引起上层海水产生垂直运动,致使上层海水热含量重新分市。
Topographic Rossby waves nonlinear interaction causes sea water vertical motion and heat content redistribution in the upper sea level .
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海洋环境的一个最典型特点就是海水处于无时无刻的运动之中,海水的各项物理性质、海洋中的各种物质也随之运动。
The typical characteristic of the ocean environment is the ever moving sea water .
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本试验可以分成两大部分:第一部分主要研究模拟自然条件下,滨海盐渍土水盐运动规律以及海水灌溉下水盐运动规律;
Simulation was conducted to study the relative movement between salt and water of seashore saline soil .
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该模型不仅考虑了质点在海水中的对流运动,而且还用大量质点的随机扩散模拟湍扩散过程。
Not only convection but also random diffusion of substantial particle and their sediment are considered in the model .
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接着用差分法计算了海水受海底地面运动激扰时的流场分布,也用分域迭代解法计算了海水-海床土耦联体系的地震反应;
Then the flow distributions of seawater disturbed by undersea ground motion are computed by a finite difference method , and the seismic responses of seawater-seabed soil coupling system are also computed by a subfield-iteration method ;
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磁流体(MHD)推进是一种新型的船舶推进方式。它利用海水中电流和磁场间的相互作用力使海水运动,其反作用力为推力,推进船舶运动。
As a new type of ship propulsion , AC Magnetohydrodynamic ( MHD ) propulsion apply alternating magnetic field through seawater , then a Lorentz force will act to move the seawater and thus drive the ship to move .
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在渤海中部的纬向断面上,东部的海水垂直交换要比西部活跃得多;渤海海水的垂向运动亦主要是密度流导致的。
On the zonal section in the central Bohai Sea , the vertical water exchange is more active in the east than in the west , and the vertical water movement in the Bohai Sea is also caused mainly by the density current .