Loading in 5 sec....

Kinematics of the horizontal wind fieldPowerPoint Presentation

Kinematics of the horizontal wind field

- 64 Views
- Uploaded on
- Presentation posted in: General

Kinematics of the horizontal wind field

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.

- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -

Kinematics of the horizontal wind field

(Kinematics: from the Greek word for ‘motion’, a description of the motion of a

particular field without regard to how it came about or how it will evolve)

y

N

V

v

W

E

u

x

S

To derive a mathematical expression for the

key kinematic properties of the wind field

we will use the coordinate system on the right.

y

We will use Taylor Expansion

to estimate the wind field at an arbitrary point

x,y from the wind at a nearby point x0, y0

x, y

x0, y0

Peform a 2D Taylor expansion:

For simplicity, lets assume that x0, y0 is the origin 0,0

And that we can obtain an adequate estimate of u,v by retaining

only the first derivatives. We are assuming that over the small distance

the u and v field vary linearly. Then…

Let’s take a simple step and write each derivative term as (for example) :

From before:

(1)

(2)

Now we will write two nonsense equations

(3)

(4)

Now we add (1) and (3). We also separately add (2) and (4). Then we

rearrange the terms and get…………

Translation

Divergence

Shearing

Deformation

Relative

Vorticity

Stretching

Deformation

Any wind field that varies linearly can be characterized by these

five distinct properties. Non-linear wind fields can be closely

characterized by these properties.

y

x

Translation

The effect of translation on a fluid element:

Change in location, no change in area, orientation, shape

y

Divergence (d > 0)

Convergence (d < 0)

The effect of convergence on a fluid element:

x

Change in area, no change in

orientation, shape, location

y

Positive (cyclonic) vorticity ( > 0).

Negative (anticyclonic) vorticity ( < 0)

The effect of negative vorticity on a

fluid element:

x

Change in orientation, no change in area, shape, location

y

E-W Stretching Deformation (D1 > 0).

N-S Stretching Deformation (D1 < 0).

The effect of stretching deformation on a

fluid element:

x

Change in shape, no change in area, orientation, location

y

SW-NE Shearing Deformation (D1 > 0).

NW-SE Shearing Deformation (D1 < 0).

The effect of shearing deformation on a

fluid element:

x

Change in shape, no change in area, orientation, location

Why are we interested in these properties?

Net Divergence in an air column leads to the development of low surface pressure

Net Convergence in an air column leads to the development of high surface pressure

L

H

Vertical vorticity (spin about a vertical axis) arises from three sources:

Horizontally sheared flow, flow curvature, and the rotation of the earth.

Relative vorticity: shear and curvature.

Absolute vorticity: shear, curvature and earth rotation.

z

< 0

z

> 0

z

< 0

z

> 0

Absolute vorticity allows us to identify short waves and shear zones within the

jetstream. Short waves trigger cyclogenesis and can help trigger deep

convection in the warm season.

Positive Vorticity Advection on a 500 mb map can be used as a proxy for divergence aloft, and is related to the development of low surface pressure and upward air motion.

T- 8DT

T- 8DT

T- 7DT

T- 7DT

T- 6DT

T- 6DT

T- 5DT

T- 5DT

T- 4DT

T- 4DT

T- 3DT

T- 3DT

T- 2DT

T- 2DT

T- DT

T- DT

T

T

Deformation flow is fundamental to the development of fronts

Time = t + Dt

Time = t

y

y

x

x

EXAMPLES OF DEFORMATION

Axis of Dilitation

EXAMPLES OF DEFORMATION

Axis of Dilitation

CONFLUENT and DIFLUENT FLOW

Is this flow convergent?

Is this flow divergent?

NO: The areas of the two boxes are identical. The flow is a combination of translation and deformation.

The terms for divergence, relative vorticity, and deformation strictly apply on a plane tangent to the earth’s surface. If we take earth’s curvature into account, we have to add an additional term.

Suppose the wind is southerly and

uniform. Is the wind convergent?

Red = wind

Blue = wind component

y

Yes!

y

y

x

x

x

Convergence of meridians toward

north leads to convergence. This

is the earth curvature term (the last term)

in the expression for convergence (d).

Suppose the wind is westerly and

uniform. Does vorticity exist?

Yes!

Convergence of meridians toward

north creates vorticity. This

is the earth curvature term (the last term)

in the expression for vorticity ().

In a similar way, convergence of the earth’s meridians toward

the north leads to deformation in otherwise uniform flow

Earth’s curvature terms are an order of magnitude smaller than other

terms, but cannot be ignored in models, at least in the middle and high

latitudes.