ATM OCN (Meteorology) 100 - Lecture 3

Answers for Homework 5

Fall 1997


The total maximum points were 60.


ATMOSPHERIC MOTIONS

1. Identify the following characteristics associated with each of the force components in the atmospheric equation of motion:

[30 pts at 2 pts each]

A. VERTICAL PRESSURE GRADIENT FORCE

  • DIRECTION:

Vertical and upward (from high pressure near the surface toward low pressure aloft, or opposite of down).

  • MAGNITUDE depends upon:

Altitude (also it depends upon the vertical spacing of the pressure surfaces, which depend upon the average temperature of the layer).

B. HORIZONTAL PRESSURE GRADIENT FORCE

  • DIRECTION:

Horizontal and upward pointed from high pressure toward low pressure (as seen on a weather chart).

  • MAGNITUDE depends upon:

Packing of the isobars on a horizontal, constant altitude weather chart.

C. GRAVITATIONAL FORCE or "GRAVITY"

  • DIRECTION:

Vertical and downward (toward the center of the earth).

  • MAGNITUDE depends upon:

The masses of the earth and the object and upon the separation between their centers (or equivalently, upon altitude).

D. CORIOLIS EFFECT or "FORCE" (Horizontal Component)

E. FRICTIONAL FORCE (Horizontal Component)

F. CENTRIPETAL FORCE


2. What is the primary physical significance of the hydrostatic balance relationship?

[4 pts]

The earth maintains an atmosphere, since large scale accelerations of air away from the earth's surface are inhibited by gravity.


3. From this hydrostatic balance relationship, how does the magnitude of the vertical pressure gradient in a warm air column compare with the vertical pressure gradient in a column of cold air?

[4 pts]

The vertical pressure gradient in a warm air column is less than in a cold air column.


4. a) What forces are balanced in the geostrophic wind model?

[4 pts.]

The horizontal components of the pressure gradient force and the Coriolis force.

b) Name three separate assumptions used to describe the geostrophic wind model.

[6 pts or 2 pts. each]

Select 3 of following 4:

1. No net acceleration

2. Frictionless

3. Straight and parallel isobars

4. Horizontal flow


5. On the horizontal surface pressure map in the Northern Hemisphere (within the friction layer), locate the regions of high and low pressure, placing a large block H and L, respectively. Make a force diagram by neatly drawing thin arrows to signify the direction and relative magnitudes of the horizontal pressure gradient force (FHPG), the Coriolis force (FCOR), the friction force (FFRC). Label each of these forces. Neatly draw a thick, double bladed arrow to represent the resultant wind (VRES); label this wind vector:

[12 pts]


Last revision 12 November 1997

Produced by Edward J. Hopkins, Ph.D.
Department of Atmospheric and Oceanic Sciences
University of Wisconsin-Madison Madison, WI 53706
hopkins@meteor.wisc.edu


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