Chapter 6: effect of Discritization Flashcards
The effect of the various discretizations in space and time may be studied systematically in the context of a
linearized model.
The effect of the various discretizations in space and time may be studied systematically in the context of a linearized model.
With such a model, it is possible to determine
analytical solutions both for the system of equations under consideration and for the system obtained after discretization
The shallow water barotropic model is used as a
a study tool
The shallow water barotropic model is used as a study tool, as it has as solutions the two types of waves described by the primitive equation models:
- slow (Rossby) waves associated with advection terms and
- fast inertia-gravity waves associated with the Coriolis terms and the adaptation terms (pressure force in the equations of motion and divergence in the continuity equation).
The equations of the linearized shallow water model are obtained from
the corresponding nonlinear equations by using the small perturbation method.
The equations of the linearized shallow water model are obtained from the corresponding nonlinear equations by using the small perturbation method.
This consists in
writing the model variables as the sum of a time-independent basic state and of perturbations evolving over time.
When using the spectral method, it can be considered that the
horizontal derivatives are evaluated exactly and that no error is made therefore (except for computer accuracy).
When using the spectral method, it can be considered that the horizontal derivatives are evaluated exactly and that no error is made therefore (except for computer accuracy).
Where finite differences are used on
a grid
Where finite differences are used on a grid, the horizontal derivatives are
not calculated exactly and a discretization error is introduced
Where finite differences are used on a grid, the horizontal derivatives are not calculated exactly and a discretization error is introduced, whose effects on ……………. must be calculated
wave propagation must be calculated.
Effects of Horizontal Discretization
For this, the advection and adaptation terms of the linearized shallow water equations are discretized on various types of grids (A-D).
Types of Grids
The A-type grid
is the simplest that can be imagined, with all the variables being expressed at the same place.
Types of Grids
In B-type grid
the velocities u and v are calculated at the locations other than that of geopotential o|
Types of Grids
The C-type grid
is characterized by the fact that the velocities u and v together with the geopotential o| are evaluated at different points.
Types of Grids
D-type grid
The idea of D-type grid is to switch around the position of the variables on passing from one time step to the next.
The idea of D-type grid is to switch around the position of the variables on passing from one time step to the next.
For even time steps the position of the variables is as with the C grid, except that the positions of velocities u and v are reversed.
• For odd time steps, all the variables switch position, the u′s take the places of the v ‘s, the v ‘s of the u′s and the geopotential o| is now calculated in the center of the grid.
Three cases of discretization are distinguished for the ………… terms
advection
Three cases of discretization are distinguished for the advection terms
- central differences on the A, B, or C grids
- discretization on the D staggered grid
- central differences of 4th-order accuracy on the A grid