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The action of warm air rising and cold air sinking (convection) plays a key role in the formation of severe thunderstorms. If the warm surface air is forced to rise, it will continue to rise, because it is less dense than the surrounding air. In addition, it will transfer heat from the land surface to upper levels of the atmosphere through the process of convection.
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Two of the most important ingredients for thunderstorm formation are instability (unstable air) and moisture. Click here to review what causes unstable air. There are three main types of thunderstorms; orographic, air mass, and frontal. |
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Frontal thunderstorms occur along the boundaries of weather fronts (e.g. cold front). |
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An intense line of thunderstorms that forms right along or just ahead of a cold front is called a squall line. Shown below is a radar image of a squall line thunderstorm. Supercell thunderstorms occur
when very strong updrafts are balanced by downdrafts. This can allow
the storm to persist for many hours. In a supercell, a moist, unstable
body of warm air may be forced to rise by an approaching cold front.
The result is a strong, persistent updraft of warm moist air. Speeds in an updraft can be as fast as 90 miles per hour! The air cools as it rises. Water vapor condenses and forms cumulus clouds. When condensation occurs, heat (latent heat/energy ) is released and helps the thunderstorm grow.
At some point, condensation high in the cloud (now in the form of water droplets and ice) falls to the ground as rain. A cold downdraft forms as the rain falls.
If conditions are right, some supercell thunderstorms will spawn tornadoes. Lets see how. |
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Return to the Thunderstorms Home Page [Thunderstorms & Tornadoes] [Hurricanes] [Blizzards & Winter Weather] [Clouds] |
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