AIR MASS CLASSIFICATION
LEARNING OBJECTIVE: Define air mass
classification
and
describe
how
the
classification will change when characteristics
modify.
Air masses are classified according to geographic
source region, moisture content, and thermodynamic
process.
Geographic Origin
The geographical classification of air masses,
which refers to the source region of the air mass,
divides air masses into four basic categories: arctic or
antarctic (A), polar (P), tropical (T), and equatorial (E).
An additional geographical classification is the
superior (5) air mass. The superior air mass is generally
found aloft over the southwestern United States, but is
sometimes located at or near the surface.
Moisture Content
The arctic (A), polar (P), and tropical (T)
classifications are further broken down by moisture
content. An air mass is considered to be maritime (m) if
its source of origin is over an oceanic surface. If the air
mass originates over a land surface, it is considered
continental (c). Thus, a moist, maritime arctic air mass
is designated m; and a drier, continental arctic air mass
is designated c. Equatorial (E) air is found exclusively
over the ocean surface in the vicinity of the equator and
is designated neither c nor m but simply E.
Thermodynamic Process
The thermodynamic classification applies to the
relative warmth or coldness of the air mass. A warm air
mass (w) is warmer than the underlying surface; a cold
air mass (k) is colder than the underlying surface. For
example, a continental polar cold air mass over a
warmer surface is classified as cPk. An mTw
classification indicates that the air mass is a maritime
tropical warm air mass and overlays a cooler surface.
Air masses can usually be identified by the type of
clouds within them. Cold air masses usually show
cumuliform clouds, whereas warm air masses contain
stratiform clouds. Sometimes, and with some air
masses, the thermodynamic classification may change
from night to day. A particular air mass may show k
characteristics during the day and w characteristics at
night and vice versa. The designators and descriptions
for the classifications of air masses are listed in table
4-1.
4-4
Designator
Description
cAk
Continental arctic air that is colder than the surface over which it lies.
cAw
Continental arctic air that is warmer than the surface over which it lies.
mAk
Maritime arctic air that is colder than the surface over which it lies.
cPw
Continental polar air that is warmer than the surface over which it is moving.
cPk
Continental polar air that is colder than the surface over which it is moving.
mPw
Maritime polar air that is warmer than the surface over which it is moving.
mPk
Maritime polar air that is colder than the surface over which it is moving.
mTw
Maritime tropical air that is warmer than the surface over which it is moving.
mTk
Maritime tropical air that is colder than the surface over which it is moving.
cTw
Continental tropical air that is warmer than the surface over which it is moving.
cTk
Continental tropical air that is colder than the surface over which it is moving.
Ek
Maritime equatorial air that is colder than the surface over which it is moving.
Ew
Maritime equatorial air that is warmer than the surface over which it is moving.
S
Superior air, found generally aloft over the southwestern United States, and occassionally at or near
the surface.
Table 4-1.Classification of Air Masses