Hybrid Eulerian and Lagrangian Simulation of Steep and Breaking Waves and Surface Fluxes in High Winds

Abstract

This research aims at developing a numerical capability using a Lagrangian Smoothed Particle Hydrodynamics (SPH) method and an Eulerian Level-Set Method (LSM) for the simulation of steep and breaking waves in high winds. The ultimate goal is to establish an advanced computational framework for the investigation of wind-wave breaking in air-sea interaction processes, including the airflow separation over steep and breaking waves, the wind wave momentum and energy transfer, the momentum and energy injection from breaking waves to the upper ocean, and the turbulence transport process. The scientific and technical objectives of this research are: (1) Develop an Eulerian and Lagrangian multi-fluids simulation capability by using the SPH and LSM with environmental input provided by coupled wind and wave simulations at far field; (2) Use the numerical method developed in (1) to simulate wind wave ocean interactions at small scales to elucidate flow structure; (3) Quantify and characterize wind wave momentum and energy transfer and the injection to the upper ocean by breaking waves; and (4) Simulate and identify key process in turbulence transport near steep and breaking waves.

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Document Details

Document Type
Technical Report
Publication Date
Sep 30, 2012
Accession Number
ADA590591

Entities

People

  • Lian Shen
  • Robert Anthony Dalrymple

Organizations

  • Johns Hopkins University

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Boltzmann Equation
  • Civil Engineering
  • Drag
  • Dynamic Pressure
  • Electrical Solitons
  • Energy
  • Energy Transfer
  • Engineering
  • Far Field
  • Flow
  • Flow Fields
  • Graphics Processing Unit
  • Measurement
  • Pressure Distribution
  • Simulations
  • Turbulence
  • Waves

Readers

  • Coastal Oceanography
  • Computational Fluid Dynamics (CFD)
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers