GIANNETTA WEATHER |
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"N O T E"
All weather articles written by the author,
weather records for Bath, Pa. USA, graphs,
graphics, pictures, are copyrighted and are owned by the author.
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Fronts |
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1. Front: A transition zone between two air masses of different
densities.
2. Density is controlled by the temperature and humidity of the air.
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Cold Fronts |
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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 |
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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.
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Warm Fronts |
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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.
© 1998 Charles A. Giannetta