Meteorology Charles A. Giannetta
Meteorologist - Professor
"Warm Fronts"
1. The edge of an advancing warm air mass is called a Warm Front.
2. Warm air rides up and over colder air since it is less dense.
3. Warm Frontal Slopes average about 1:200 miles. This means that when
the warm front is located on the surface, 200 miles ahead of it
the warm air is about 1 mile up.
4. Warm Fronts usually move about 15 to 20 mph.
"Stationary Fronts"
1. When opposing forces of adjacent air masses of different densities
are
such that the frontal surface between them shows little or no
movement, is called a Stationary Front.
2. Stationary Fronts move less than 6 mph.
3. The winds usually blow parallel on both sides of a Stationary Front:
Example: East to West on the north side of the front, and West to
East
on the south side of the front.
"Occluded Fronts"
1. There are 2 types of Occluded Fronts. Cold Air Occlusion and Warm
Air Occlusion.
2. Occluded means to close or come together.
3. When fronts occlude, the weather system is beginning to dissipate.
4. Cold Air Occlusion: When cold air overtakes and replaces warm air.
5. Warm Air Occlusion: When warm air overtakes and replaces the colder
air.
1. World War I: It was during WWI Norwegion meteorologists discovered
and named fronts after the battlefronts of the war.
2. Overrunning: When warmer less-dense air flows up and over colder
more-dense surface air.
3. Back Door
Cold Fronts: Most cold fronts generally move from northwest to the
Cold Fronts: southeast. There are times when a cold
front will move from the northeast portion of the
United States to the southwest. When this occurs,
these fronts bring with them a welcome relief from
hot weather in the summer. During the winter the weather
becomes cold and dank.