ch2: finite differences (part-B) Flashcards

1
Q

As the space difference schemes are used to

A

march forward in space

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

As the space difference schemes are used to march forward in space, in NWP, to march forward in time, one needs to

A

use a time differencing scheme.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Unlike space differencing schemes, time differencing schemes seem to

A

meet the accuracy requirements at the first and second order.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Higher order schemes appear

A

cumbersome and are not of wide use in NWP.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

The forward and centered time difference formulae are expressed as:

A
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

There exist two basic types of temporal differencing schemes:

A

explicit and implicit schemes.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

With explicit schemes,

A

a model prognostic equation is approximated using finite differences in such a way that variables at the future time appear only on one side of an equation.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

With explicit schemes, a model prognostic equation is approximated using finite differences in such a way that variables at the future time appear only on one side of an equation. For example, consider the following 1‐D wave equation:

A
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

the above is

A

eapfrog time differencing, in which the variable u at the future time appears only on one side (LHS) of the equation, is an example of explicit scheme.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

How the leapfrog time differencing scheme works in practice?

A
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

implicit methods

A

variables at the future time appear on both sides of the equation and require the use of iterative methods to solve

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

implicit methods, variables at the future time appear on both sides of the equation and require the use of iterative methods to solve.

 Consider again the

A

simple 1‐D advection equation for u and apply a backward finite difference in time and centered finite difference in space to obtain:

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

For the time differencing schemes to produce numerically‐stable solutions, there exists

A

a limiting value of what is known as the Courant number:

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

The Courant number is

A

non‐dimensional, where U is the translation speed of the fastest feature or wave on the model grid, Δx is the horizontal grid spacing, and Δt is the time step.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

CFL condition

A

The limiting value of the Courant number is known as the CFL condition, representing the maximum value of the Courant number that permits numerically‐stable model solutions.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

The exact value of the CFL condition varies depending upon

A

the spatial and temporal finite different scheme utilized

17
Q

he exact value of the CFL condition varies depending upon the spatial and temporal finite different scheme utilized; however, a general guideline is that:

A
18
Q

Choosing fine grid spacing results in

A

small time steps between intermediate forecasts leading to an increase in the no. of time steps and computing time.

19
Q

What should be the time step for the following grid spacing when the speed of

the fastest wave in the model is 18 m/s?

A
20
Q

What should be the time step for the following grid spacing when the speed of

the fastest wave in the model is 18 m/s?

Thus, according to CFL condition,

A

ine‐mesh (smaller grid size) model forecasts require more number of intermediate time steps and thus need powerful computers.

21
Q

equation gives the time changes in moisture at any grid point (x,y) due to moisture advection in x‐direction.

A
22
Q
A

Consider the 1D moisture advection equation as shown

The above equation gives the time changes in moisture at any grid point (x,y)

due to moisture advection in x‐direction.

23
Q

how to obtain the forecasting variable

A
24
Q

For a grid space of ∆x=25 km, substitute the given values of q at a time t and obtain its forecast value after 1 hour. Consider the speed of the fastest wave in the model grid as 12 m/s.

A