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In this paper an evoluion equation in integral-differential form for finite amplitude Rossby waves on a weak shear is presented and an efficient method for its numerical solution is set up. It is shown that a propagation of solitary wave is possible whenever a proper weak shear in basic flows acts with the nonlinear effects and dispersion of the media, both in the atmosphere and in the ocean. To test the numerical method for solving the evolution equation, a series of experiments are carried out. The results indicate that the solitary solutions, do exist and interact with each other in quite a succinct, manner. Therefore the method is successful and efficient for solving initial value problems of the above equation. The time decoupling problem arising in the numerical scheme and the related filtering technique are discussed. A variety of interesting phenomena such as the interaction of solitary Rossby waves, damping, dispersion and the development of nonlinear wave train are numerically studied. 相似文献
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边界元方法(BEM)是近代计算力学中的一种高效数值方法。由于采用相应的边界积分方程,使处理的问题减少了一维,从而给出的方程组就小得多,要求输入的数据也就大大地减少了,而所得结果的精度却高于有限元法。因此边界元法对于所谓的“区域法”,例如有限差分法(FDM)和有限元法(FEM)具有很强的竞争能力。 大量应用表明:边界元法与有限元法相比,不仅经济、易于使用,而且在许多工程领域,包括某些海洋参数的数值分析和预报方面都是很有发展前途的。 本文首先介绍了边界元方法的基本思想、数学原理和实施步骤,然后分别说明如何将这种方法用于更复杂的、非线性的、依时的问题。最后将讨论边界元法在一般粘性流体流动中的应用。 相似文献
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三、广义Green公式 当描述物理问题的控制方程不是Laplace方程时,就不可能由Green第二恒等式(2)来建立相应的边界积分表示式了,这时需要采用广义Green公式。 设某个物理问题在以Γ为边界的区域Ω内可由下列偏微分方程描述 相似文献
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