accounts for the increases in gradients. In tropical
regions, the geostrophic wind scales become less
reliable because pressure gradients are generally rather
weak.
REVIEW QUESTIONS
Q3-1. Which two factors influence the Earth's
temperature?
Q3-2. What are the major factors that result in the
wide distribution of pressure over the earth's
surface?
Q3-3. What effect does Coriolis force have on
thermal
circulation
in
the
Northern
Hemisphere?
Q3-4. According to the 3-cell theory, how many
circulation belts are there?
Q3-5.
According to the 3-cell theory, what type of
pressure system would you normally find at
30 degrees north latitude?
Q3-6.
What is the predominant wind system in the
tropics?
Q3-7.
Name two types of pressure gradient.
Q3-8.
What is the difference between centrifugal
force and centripetal force?
Q3-9.
What is the difference between gradient wind
and geostrophic wind?
Q3-10.
What is the relationship between centrifugal
force and pressure gradient force around
anticyclones?
SECONDARY CIRCULATION
LEARNING OBJECTIVE: Determine how
centers of action, migratory systems, and
seasonal variations affect secondary air
circulations.
Now that you have a picture of the general
circulation of the atmosphere over Earth, the next step
is to see how land and water areas offset the general
circulation. The circulations caused by the effect of
Earths surfaces, its composition and contour, are
known as secondary circulations. These secondary
circulations give rise to winds that often cancel out the
normal effect of the great wind systems.
There are two factors that cause the pressure belts
of the primary circulation to break up into closed
circulations of the secondary circulations. They are the
non-uniform surface of the earth and the difference
between heating and cooling of land and water. The
surface temperature of oceans changes very little
during the year. However, land areas sometimes
undergo extreme temperature changes with the seasons.
In the winter, large high-pressure areas form over the
cold land and the low-pressure areas form over the
relatively warm oceans. The reverse is true in summer
when highs are over water and lows form over the
warm land areas. The result of this difference in heating
and cooling of land and water surfaces is known as the
thermal effect.
Circulation systems are also created by the
interaction of wind belts of pressure systems or the
variation
in
wind
in
combination
with
certain
distributions of temperature and/or moisture. This is
known as the dynamic effect. This effect rarely, if ever,
operates alone in creating secondary systems, as most
of the systems are both created and maintained by a
combination of the thermal and dynamic effects.
CENTERS OF ACTION
The pressure belts of the general circulation are
rarely continuous. They are broken up into detached
areas of high and low pressure cells by the secondary
circulation. The breaks correspond with regions
showing differences in temperature from land to water
surfaces. Turn back to figures 3-2A and 3-2B. Compare
the temperature distribution in views A and B of figures
3-2 to the pressure distribution in views A and B of
figure 3-3. Note the gradient over the Asian Continent
in January. Compare it to the warmer temperature over
the ocean and coastal regions. Now look at view A of
figure 3-3 and note the strong region of high-pressure
corresponding to the area. Now look at the same area in
July. Note the way the temperature gradient flattens out
and warms. Look at view B of figure 3-3 and see the
low-pressure area that has replaced the high-pressure
region of winter. These pressure cells tend to persist in a
particular area and are called centers of action; that is,
they are found at nearly the same location with
somewhat similar intensity during the same month each
year.
There is a permanent belt of relatively low pressure
along
the
equator
and
another
deeper
belt
of
low-pressure paralleling the coast of the Antarctic
Continent. Permanent belts of high pressure largely
encircle Earth, generally over the oceans in both the
Northern and Southern Hemispheres. The number of
centers of action is at a maximum at about 30 to 35
degrees from the equator.
3-14