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An Ocean Circulation Model Based on Operator-Splitting, Hamiltonian Brackets, and the Inclusion of Sound Waves

机译:基于分流,哈密顿括号和声波包含的海洋环流模型

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摘要

This paper offers a simple, entirely prognostic, ocean circulation model based on the separation of the complete dynamics, including sound waves, into elementary Poisson brackets. For example, one bracket corresponds to the propagation of sound waves in a single direction. Other brackets correspond to the rotation of the velocity vector by individual components of the vorticity and to the action of buoyancy force. The dynamics is solved by Strang splitting of the brackets. Key features of the method are the assumption that the sound waves propagate exactly one grid distance in a time step and the use of Riemann invariants to solve the sound-wave dynamics exactly. In these features the method resembles the lattice Boltzmann method, but the flexibility of more conventional methods is retained. As in the lattice Boltzmann method, very short time steps are required to prevent unrealistically strong coupling between the sound waves and the slow hydrodynamic motions of primary interest. However, the disadvantage of small time steps is more than compensated by the model's extreme simplicity, even in the presence of very complicated boundaries, and by its massively parallel form. Numerical tests and examples illustrate the practicality of the method.
机译:本文基于将包括声波在内的完整动力学分离为基本的Poisson括号,提供了一个简单的,完全可预测的海洋环流模型。例如,一个括号对应于声波在单个方向上的传播。其他括号对应于涡旋各个分量的速度矢量的旋转以及浮力的作用。通过括号的Strang拆分解决动力学问题。该方法的主要特征是假设声波在一个时间步长内精确地传播一个网格距离,并使用黎曼不变式精确地解决声波动力学问题。在这些特征中,该方法类似于格子Boltzmann方法,但保留了更多常规方法的灵活性。像在格子玻尔兹曼方法中一样,需要非常短的时间步长才能防止声波与主要关注的缓慢流体动力运动之间出现不切实际的强烈耦合。但是,时间步长较小的缺点甚至可以通过模型的极端简单性(甚至在存在非常复杂的边界的情况下)和其大规模并行形式来弥补。数值测试和算例说明了该方法的实用性。

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  • 来源
    《Journal of Physical Oceanography 》 |2009年第7期| 1615-1633| 共19页
  • 作者

    Rick Salmon;

  • 作者单位

    Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California UCSD Dept. 0213, 9500 Gilman Drive, La Jolla, CA 92093-0213;

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  • 正文语种 eng
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