Title: Modeling Ocean Currents in COMSOL
1Modeling Ocean Currents in COMSOL
- Reza Malek-Madani
- Kevin McIlhany
- U. S. Naval Academy
- 24 Oct, 2006
- rmm_at_usna.edu
2CCBOM
- Center for Chesapeake Bay Observation and
Modeling - Mathematics
- Oceanography
- Physics
- Ocean Engineering
- Chemistry
Acoustic Wave and Current Profiler (AWAC)
3Velocity 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
4dx/dt u(x, y, z, t), dy/dt v(x, y, z, t)
5Bathymetry
6Deformation in MATLAB (N. Brasher, RMM, G.
Fowler)
7Particle 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
9Goals 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
10Stommels model
1948 paper, Key Assumptions 2D, Steady,
Rectangular Basin, Bottom Friction Key Features
Wind stress, Coriolis Key Findings Boundary
Layer (Gulf Stream)
Boundary conditions ? 0 on all four boundaries
Scales N. Atlantic Basin 10,000 Km by 6000
Km Depth 200 Meters Coriolis Parameter 10(-13)
11Munks Model
Zero boundary conditions
Multiphysics approach
12Non Rectangular Geometries
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