Cirrus cloud Totally Explained

Everything about Cirrus Cloud totally explained

Cirrus clouds are characterized by thin, wisplike strands, often accompanied by tufts, leading to their common (non-standard) name of 'mare's tail'. Sometimes these brownish clouds are so extensive that they're virtually indistinguishable from one another, forming a veil or sheet called "cirrostratus". Sometimes convection at high altitudes produces another form of cirrus called "cirrocumulus", a pattern of small cloud tufts which include droplets of supercooled water.
   Many cirrus clouds produce hair like filaments made of the heavier [ice] crystals that precipitate from them. These "fall streaks", a form of virga, often indicate the difference in the motion of air (wind shear) between the upper part of the cirrus cloud and the air below it. Sometimes the top of the cirrus cloud is moving rapidly above a slower layer of air, or the streak is falling into a faster moving lower layer. The directions of these winds can also vary.
   Cirrus usually form at altitudes above 8000 meters (26,000 ft). At this altitude, aircraft leave condensation trails that can turn into cirrus clouds. This happens when hot exhaust, mostly water, freezes leaving a visible trail. Streaks may appear straight when wind shear is absent, giving the clouds the appearance of a comma (cirrus uncinus), or tangle, an indication of high-level turbulence. The falling ice crystals evaporate before reaching the ground.
   Cirrus clouds trap and reflect infrared radiation (heat) beneath them (greenhouse effect), but also reflect sunlight to some extent (albedo). It hasn't yet been determined whether the net effect of cirrus clouds is to warm or cool the earth. Much of the difficulty lies in modeling the albedo effect of clouds composed of various size and shape crystals. Older models tend to underestimate the albedo effect of cirrus. Refinements of these models will improve climate predictions.
   Cirrus Clouds can be light or dark - Bella
   If there are many cirrus clouds in the sky, this may be a sign that a frontal system or upper air disturbance is approaching; usually meaning the weather will change within the next 24 hours. Cirrus clouds can also be the remnants of a thunderstorm. A large shield of cirrus and cirrostratus typically accompany the high altitude outflow of hurricanes/typhoons. Cirrus clouds have also been observed to develop after the persistent formation of contrails from aircraft.

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