Lesson
Content
General ciculation of the atmosphere is important to know to be
aware of the large scale patterns of the atmosphere. For flying,
it is particular to know about airmasses and fronts. Some summary
information on these topics is presented below.
Airmass
An air mass is an extremely large body of air whose properties of temperature and moisture content (humidity) are
similar in any horizontal direction. Air masses can cover hundreds
of thousands of square miles. Air masses are formed when
air stagnates for long periods over a uniform surface. The
characteristic weather features (temperature and moisture) of
air masses are therefore determined by the surface over
which they form. An air mass acquires these attributes through
heat and moisture exchanges with the surface. As a result, an air mass
can be warm or cold and moist or dry.
More on airmasses
[back to
top]
Fronts
Although an individual air mass can change over time, different air masses do
not mixreadily. Therefore, when two air masses come in close contact they retain
their
separate identities for several days. The transition zone between two different
air masses
is called a front. Fronts can be hundreds of miles long and exist as long as
the air masses
they separate remain distinct.
Norwegian meteorologists around the time of World War I laid the
foundation for our concepts of fronts and their movements. They
observed large air masses with different temperature and moisture
properties that advanced and retreated versus one another. Clashing
air masses often led to disruptive weather conditions. The boundary
between air masses was called a “front,” analogous to the boundaries
used on military maps to separate battling armies.
More on Fronts.
[back to
top]
Global
circulation summary
Upward vertical motions near the equator explain the Intertropical
Convergence Zone (ITCZ), which can be identified in global satellite
imagery and precipitation maps. When rising air reaches the tropopause
and moves poleward, it comes closer to the Earth’s axis of rotation
and increases speed to conserve angular momentum. This produces the
subtropical jet stream.
The descending air of the Hadley cell is compressed and warms,
lowering the relative humidity. This sinking air explains the large
deserts of Africa, Saudi Arabia, and Australia. The sinking air
of the Hadley cell results in calm winds at the surface, producing the “horse
latitudes” dreaded by ancient mariners who used wind power
to travel. Some descending air that reaches the surface moves toward the equator to supply moisture to the ITCZ. As air
moves toward the equator, the Coriolis force acts to produce the steady northeast and southwest trade winds sought by sailors.
Some of the air associated with the descending branch of the Hadley
cell moves poleward and clashes with cold polar air masses that
are moving toward the equator. Fronts exist where the cold air meets
the warm subtropical air, producing mid-latitude storms that tend
to move from west to the east. These storms are embedded in the
mid-latitude westerlies, causing them to move eastward. The polar
jet stream exists in the vicinity of fronts.
In our simple conceptual model the globe is covered with water—a
good approximation, because water covers 70% of the Earth’s
surface. However, the differences between land and water are important
in weather and climate.
[back to
top]
|