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Computational Studies of Three-Dimensional Ocean Sound Fields in Areas of Complex Seafloor Topography and Active Ocean Dynamics

机译:复杂海底地形和活动海洋动力学三维海洋声场的计算研究

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摘要

Time-evolving three-dimensional (four-dimensional) numerical modeling of sound is performed for ocean environmental conditions calculated using regional ocean flow models. The flow models solve the appropriate nonlinear equations in bands of resolved scales and frequencies. Subgrid scale processes are parameterized, as are boundary processes. The ocean fields are interpolated onto acoustic model grids that are two orders of magnitude tighter than the flow model grids. The computations provide reliable estimates of the acoustic effects of the resolved ocean processes such as geostrophic currents, mixed-layer changes, and internal tides, but they do not include the acoustic implications of unresolved structures such as nonlinear internal waves, sharp boundary layers, and small-scale intrusions. Examples of complicated sound fields from resolved and unresolved features will be presented, and prospects for applying the methods will be discussed.
机译:对于使用区域洋流模型计算出的海洋环境条件,进行了声音的时变3维(4维)数值模拟。流动模型在已解决的比例和频率范围内求解适当的非线性方程。子网格规模的过程以及边界过程都是参数化的。将海洋场内插到比流动模型网格紧两个数量级的声学模型网格上。这些计算提供了对已解析海洋过程的声学效应的可靠估计,例如地转流,混合层变化和内部潮汐,但它们不包括未解析结构的声学影响,例如非线性内部波,尖锐边界层和小规模入侵。将给出来自已解析和未解析特征的复杂声场示例,并将讨论应用该方法的前景。

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