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Click here to Order your Radar Equipment Online FAST-MOVING COLD FRONTS (INACTIVE COLD FRONT) The fast-moving cold front is a very steep front that has warm air near the surface being forced vigorously upward. At high levels, the warm air is descending downward along the frontal surface. This front has a slope of 1:40 to 1:80 miles and usually moves rapidly; 25 to 30 knots may be considered an average speed of movement, They move with 80 to 90 percent of the wind component normal to the front. As a result of these factors, there is a relatively narrow but often violent band of weather.Figure 4-3-2 shows a vertical cross section of a fast-moving cold front with resultant weather. Also indicated in the lower half of the diagram is the surface weather in advance of the front and the upper airflow above the front.If the warm air is moist and unstable, a line of thunderstorms frequently develops along this front. Sometimes, under these conditions, a line of strong convective activity is pro-jected 50 to 200 miles ahead of the front and parallel to it. This may develop into a line of thunderstorms called a squall line. On the other hand, when the warm air is stable, an overcast layer of altostratus clouds and rain may extend over a large area ahead of the front. If the warm air is very dry, little or no cloudiness is associated with the front. The front depicted is a typical front with typical characteristics.The fast-moving cold front is considered an INACTIVE front because lifting occurs only at and ahead of the front. The lifting is caused by descending air ahead of the front and only in part by the frontal surface.Surface Characteristics Pressure tendencies fall ahead of the front with sudden and strong rises after frontal passage.Weather Cumulonimbus clouds are observed along |
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