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Although there are different scenarios that might produce a cirrus cloud, they are often found in advance of a warm front. The warm air rides up on the cooler air as it moves. The actual meeting of the air masses is higher in the atmosphere in advance of the ground location of the front. As the warm air rises a combination of dropping pressure and dropping temperature (adiabatic cooling) causes the water vapor to change state. Because warmer air is less dense, it tends to remain above the cooler air mass.

The highest clouds are cirroform clouds. These clouds are made up of ice crystals and are found at 6-12 km. This group includes cirrus clouds, which are observed from the surface as thin hooks and strands. While cirrus clouds are easily observed from the surface, they are usually so thin that they are difficult to detect by satellite. In strong thunderstorms, however, strands of thicker cirrus clouds are often visible as outflow at the top of the thunderstorm. Cirrus clouds are very helpful in determining the direction of upper-level winds. The cloud strands, when visible, are oriented parallel to the upper level winds. Dense cirrus decks can be observed in visible images as streaks or bands and can be distinguished from lower clouds by the shadow they cast below. In the infrared image, the denser cirrus are very bright because of their cold temperature, but can be subject to the effects of a heterogeneous field of view.

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16y ago
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15y ago

no cirrus does not cause weather.

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Q: Will it rain soon if you see a cirrus cloud?
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nothing much


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