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Modeling Ocean Currents in COMSOL

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Velocity Vector Field, Chesapeake Bay, Dec 27, 1999, ... Complex Geometries: 2D and 3D boundaries of the Chesapeake Bay. Eigenvalue and Poisson Solvers ... – PowerPoint PPT presentation

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Title: Modeling Ocean Currents in COMSOL


1
Modeling Ocean Currents in COMSOL
  • Reza Malek-Madani
  • Kevin McIlhany
  • U. S. Naval Academy
  • 24 Oct, 2006
  • rmm_at_usna.edu

2
CCBOM
  • Center for Chesapeake Bay Observation and
    Modeling
  • Mathematics
  • Oceanography
  • Physics
  • Ocean Engineering
  • Chemistry

Acoustic Wave and Current Profiler (AWAC)
3
Velocity Vector Field, Chesapeake Bay, Dec 27,
1999, Courtesy of Tom Gross, NOAA, Coastal
Survey Division http//chartmaker.ncd.noaa.gov/csd
l/op/images/UVanim.gif
4
dx/dt u(x, y, z, t), dy/dt v(x, y, z, t)
5
Bathymetry
6
Deformation in MATLAB (N. Brasher, RMM, G.
Fowler)
7
Particle Fate in MATLAB
8
  • How do the errors in the velocity field affect
    the errors in the dynamical systems computations
    and the particle fates?
  • Are the statistics of the particle trajectories
    stable and realizable relative to the statistics
    of the velocity field?
  • Are stable and unstable manifolds of the system
    dx/dt u, dy/dt v computable if u and v are
    known only locally in time (90 day date length)
    and in space (incomplete data collection)?
  • New hydrodynamic model

9
Goals and Strategy
  • Goals
  • Obtain velocity field for the dynamics of the
    Chesapeake Bay, based on real wind and planetary
    forcing, and
  • Apply dynamical systems tools to the velocity
    field to understand transport and mixing in the
    Bay.
  • Strategy First consider reduced models.
  • Qualitative Models Simple geometry Emphasis
    on PDEs - Stommel, Munk, Veronis, 2 1/2 layer
    model, Navier-Stokes, nonlinear Ellipitic PDEs
  • Complex Geometries 2D and 3D boundaries of the
    Chesapeake Bay. Eigenvalue and Poisson Solvers
  • Comparison With Quoddy (NOAA) model

10
Stommels model
1948 paper, Key Assumptions 2D, Steady,
Rectangular Basin, Bottom Friction Key Features
Wind stress, Coriolis Key Findings Boundary
Layer (Gulf Stream)
  • stream function

Boundary conditions ? 0 on all four boundaries
Scales N. Atlantic Basin 10,000 Km by 6000
Km Depth 200 Meters Coriolis Parameter 10(-13)
11
Munks Model
Zero boundary conditions
Multiphysics approach
12
Non Rectangular Geometries
13
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