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Meteorology        Charles A. Giannetta
                  Meteorologist - Professor 

"F R O N T S"

1. Front: A transition zone between two air masses of different densities. 2. Density is controlled by the temperature and humidity of the air. Cold Fronts

"Cold Fronts"

1. Cold Fronts slope on the average 1:80 miles. This means that 80 miles into the surface position of the front, the frontal boundary is about 1 mile above the ground. 2. Cold Fronts may be divided into 2 types: Fast moving and slow moving. 4. A fast moving Cold Front may move along at 50 to 60+ mph. 5. Cold Fronts usually move faster in winter than summer. 6. The average speed of a Cold Front is about 30 mph.

" Squall Lines"

1. A Squall Line is an area some 50 to 200 miles ahead of a front. 2. It is characterized by a formidable wall of turbulent clouds building to 40,000 feet or higher. 3. Squall Lines contain some of the most violent and turbulent weather known. 4. Squall Lines are usually parallel to a front.






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.


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