Fronts are given their name because they are the battle zone between two different air masses. They can be identified by any of the following characteristics: a sharp temperature gradient, a sharp moisture gradient, or a sharp change in wind direction. Fronts are categorized according to their net movement. For example, when a warm air mass advances on a cooler air mass, the boundary between them is called a warm front. Clouds and light to moderate precipitation usually form ahead of a warm front. When a cold air mass advances on a warmer air mass, the boundary is called a cold front. Since surface friction creates a much steeper
slope in a cold front than in a warm front, air masses are lifted more rapidly and clouds grow to greater vertical extent. A narrow but heavy band of precipitation is usually seen along a cold front.
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