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Numerical method for tsunami calculation using full Navier-Stokes equations and the volume of fluid method.

机译:使用完整的Navier-Stokes方程和流体体积法进行海啸计算的数值方法。

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摘要

A two-dimensional numerical model was developed to study tsunami wave generation, propagation and runup. The model is based on solving the Navier-Stokes (NS) equations. The free-surface motion is tracked using the Volume of Fluid technique. The finite difference two-step projection method is used to solve NS equations and the forward time difference method to discretize the time derivative. A structured mesh is used to discretize the spatial domain. The model has been conceived as a versatile, efficient and practical numerical tool for tsunami computation, which could address a comprehensive understanding of tsunami physics with the ultimate aim of mitigating tsunami hazards. The prediction capability of tsunami generation, propagation and runup is improved by including more accurately the effects of vertical velocity/acceleration, dispersion and wave breaking. The model has the capability to represent complex curved boundaries within a Cartesian grid system and to deal with arbitrary transient-deformed moving boundaries. The numerical model was validated using laboratory experiments and analytical solutions. The model was used as a tool to determine the adequacy of the shallow water (SW) approximation in the application of tsunami simulations. Numerical results were compared with experimental data, analytical solutions and SW results in terms of the time-history free surface elevations and velocity. Reasonable agreements were observed based on the spatial and temporal distributions of the free surface and velocity.
机译:建立了一个二维数值模型来研究海啸波的产生,传播和运行。该模型基于求解Navier-Stokes(NS)方程。使用“流体体积”技术跟踪自由表面运动。有限差分两步投影法用于求解NS方程,正向时差法用于离散时间导数。结构化网格用于离散空间域。该模型被认为是用于海啸计算的通用,高效和实用的数值工具,可以解决对海啸物理学的全面了解,最终目的是减轻海啸危害。通过更准确地包括垂直速度/加速度,色散和波浪破碎的影响,提高了海啸产生,传播和运行的预测能力。该模型具有表示笛卡尔网格系统中复杂的弯曲边界并处理任意瞬态变形的移动边界的能力。使用实验室实验和分析解决方案对数值模型进行了验证。该模型用作确定海啸模拟应用中浅水(SW)近似值的适当性的工具。将数值结果与实验数据,解析解和SW结果进行了比较,得出了时程自由表面高程和速度。根据自由表面和速度的时空分布,观察到合理的一致性。

著录项

  • 作者

    Horrillo, Juan J.;

  • 作者单位

    University of Alaska Fairbanks.;

  • 授予单位 University of Alaska Fairbanks.;
  • 学科 Physical Oceanography.;Physics Fluid and Plasma.
  • 学位 Ph.D.
  • 年度 2006
  • 页码 180 p.
  • 总页数 180
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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