Chapter 6: effect of Discritization Flashcards

1
Q

The effect of the various discretizations in space and time may be studied systematically in the context of a

A

linearized model.

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2
Q

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

A

analytical solutions both for the system of equations under consideration and for the system obtained after discretization

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3
Q

The shallow water barotropic model is used as a

A

a study tool

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4
Q

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:

A
  • 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).
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5
Q

The equations of the linearized shallow water model are obtained from

A

the corresponding nonlinear equations by using the small perturbation method.

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6
Q

The equations of the linearized shallow water model are obtained from the corresponding nonlinear equations by using the small perturbation method.

 This consists in

A

writing the model variables as the sum of a time-independent basic state and of perturbations evolving over time.

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7
Q

When using the spectral method, it can be considered that the

A

horizontal derivatives are evaluated exactly and that no error is made therefore (except for computer accuracy).

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8
Q

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

a grid

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9
Q

Where finite differences are used on a grid, the horizontal derivatives are

A

not calculated exactly and a discretization error is introduced

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10
Q

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

A

wave propagation must be calculated.

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11
Q

Effects of Horizontal Discretization

A

For this, the advection and adaptation terms of the linearized shallow water equations are discretized on various types of grids (A-D).

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12
Q

Types of Grids

The A-type grid

A

is the simplest that can be imagined, with all the variables being expressed at the same place.

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13
Q

Types of Grids

In B-type grid

A

the velocities u and v are calculated at the locations other than that of geopotential o|

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14
Q

Types of Grids

The C-type grid

A

is characterized by the fact that the velocities u and v together with the geopotential o| are evaluated at different points.

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15
Q

Types of Grids

D-type grid

A

The idea of D-type grid is to switch around the position of the variables on passing from one time step to the next.

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16
Q

The idea of D-type grid is to switch around the position of the variables on passing from one time step to the next.

A

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.

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17
Q

Three cases of discretization are distinguished for the ………… terms

A

advection

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18
Q

Three cases of discretization are distinguished for the advection terms

A
  • 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
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19
Q

Results indicate that the effects of discretization appear for

A

the shorter waves only and become negligible when λ = 16Δx.

20
Q

Discretization of 4th-order accuracy has a clear advantage, although this is offset by

A

the greater volume of computation required.

21
Q

………… -grid gives better accuracy than using the ……………….

A

D-grid gives better accuracy than using the A, B, and C grids.

22
Q

Four types of discretization are distinguished for the ……….. terms:

A

adaptation

23
Q

Four types of discretization are distinguished for the adaptation terms:

A
  • central differences on the A grid
  • discretization on the B grid
  • central differences on the C or D’ grids,
  • 4th-order accuracy central differences on the A grid
24
Q

Results show that the effect of spatial discretization is fairly similar to

A

what is observed for slow waves.

25
Q

It is observed that the C or D grids provide greater accuracy than

A

the B grid, which in turn provides greater accuracy than the A grid.

26
Q

It is observed that the C or D grids provide greater accuracy than the B grid, which in turn provides greater accuracy than the A grid.

 Here again it is seen that at the cost of additional computation, the

A

4th-order accuracy discretization outclasses the 2nd-order accuracy discretizations.

27
Q

To study the properties of time discretization only, we assume that

A

the horizontal derivatives are computed exactly by the spectral method.

28
Q

Euler scheme

A

It can be shown that the Euler scheme, while decelerating waves, increases their amplitude from one time step to the next, the most prominent effect being for fast inertia-gravity waves.

29
Q

It can be shown that the Euler scheme, while decelerating waves, increases their amplitude from one time step to the next, the most prominent effect being for fast inertia-gravity waves.

• Therefore, the Euler scheme is

A

unconditionally unstable; its use in numerical prediction is reserved strictly to the first time step.

30
Q

Therefore, the Euler scheme is unconditionally unstable; its use in numerical prediction is reserved strictly to the first time step.

• The faster the …………………. the ……………………..

A

inertia-gravity waves, the more prominent the effect.

31
Q

The centered explicit scheme is

A

conditionally stable

32
Q

The centered explicit scheme is conditionally stable, the constraint on the …………………… depend essentially on ………………………………………

A

time step (CFL condition) depend essentially on the speed of the inertia-gravity waves.

33
Q

The centered explicit scheme is conditionally stable, the constraint on the time step (CFL condition) depend essentially on the speed of the inertia-gravity waves. When it is stable, it

A

accelerates the waves slightly, but preserves their amplitude.

34
Q

The centered explicit scheme is conditionally stable, the constraint on the time step (CFL condition) depend essentially on the speed of the inertia-gravity waves. When it is stable, it accelerates the waves slightly, but preserves their amplitude.

 However, because it utilizes

A

three time levels

35
Q

However, because it utilizes three time levels, it introduces in addition to

A

physical solutions, spurious solutions known as computational solutions that need to be brought under control in a model when it is integrated.

36
Q

The centered semi-implicit scheme is implemented by

A

evaluating the time derivative in central differences, the advection, and Coriolis terms at time t and by calculating the adaptation terms as the arithmetic mean of their values at time levels t + Δt and t − Δt.

37
Q

The semi-implicit scheme is

A

conditionally stable,

38
Q

The semi-implicit scheme is conditionally stable, the constraint on

A

the time step arising essentially from the velocity of the basic wind.

39
Q

The semi-implicit scheme is conditionally stable, the constraint on the time step arising essentially from the velocity of the basic wind. When it is stable, it

A

slightly accelerates the speed of slow waves, but considerably reduces the speed of inertia-gravity waves while conserving their amplitude

40
Q

The semi-implicit scheme is conditionally stable, the constraint on the time step arising essentially from the velocity of the basic wind. When it is stable, it slightly accelerates the speed of slow waves, but considerably reduces the speed of inertia-gravity waves while conserving their amplitude.

 It also introduces,

A

spurious computational solutions

41
Q

Time filtering is used to

A

attenuate (reduction of the amplitude) the decoupling between even time steps and odd time steps brought about by the existence of the computational solution in central difference schemes,

42
Q

Time filtering is used to attenuate (reduction of the amplitude) the decoupling between even time steps and odd time steps brought about by the existence of the computational solution in central difference schemes, which uses

A

the values of the variables at three successive time levels (e.g., semi-implicit centered schemes).

43
Q

In continuous filtering procedure, the values of the

A

variable at a time step are calculated using the filtered values of the previous time step successively.

44
Q

Suppose that we know the filtered values at time t − Δt, noted X (t − Δt), the values at time t + Δt are calculated first: the filtering is then applied to

A

the values at next time steps successively.

45
Q

the filtering is then applied to the values at next time steps successively.

 Introducing filtering gives a more

A

restrictive CFL stability condition

46
Q

Introducing filtering gives a more restrictive CFL stability condition. The higher the

A

wavenumber k (and therefore the shorter the wavelength), the more attenuated is the physical solution and the computational solution is itself attenuated much more than the physical solution.