CIRRUS CLOUDS - GEOGRAPHY

News: Weather Words: 'Goat's Hair’

 

What's in the news?

       Israeli researchers have uncovered a compelling connection between thunderstorms and the proliferation of wispy cirrus clouds, potentially accelerating global warming.

 

Cirrus Clouds:

       They are delicate, feathery clouds that are made mostly of ice crystals.

       They are thin and wispy in appearance, often appearing as delicate, high-altitude filaments or strands.

       Their wispy shape comes from wind currents, which twist and spread the ice crystals into strands.

       They are usually white or have a light grey colour. In the daytime, they are whiter than any other cloud in the sky.

       They are commonly known as "mare's tails" because they are shaped like the tail of a horse.

       Typically found at heights greater than 20,000 feet (6,000 metres), cirrus clouds are composed of ice crystals that originate from the freezing of supercooled water droplets.

       They generally occur in fair weather and point in the direction of air movement at their elevation.

 

Go back to basics:

High Clouds:

       They can reach above 6000 meters or 20,000 feet.

       They are also known as Cirrus Clouds.

       They are usually thin and are made up of ice.

       They often indicate fair weather and hence do not produce rain.

 

Middle Clouds:

       They form between 6,500 feet and cirrus level or from 2000 to 6000 meters.

       They are also known as “Alto” clouds.

       They frequently indicate an approaching storm.

       They may sometimes produce Virga, which is rain or snow that does not reach the ground.

 

Low Clouds:

       They lie below 6,500 feet, which means from the surface to 2,000 meters.

       They are also known as Stratus Clouds.

       They may appear dense, dark, and rainy (or snowy) and can also be cottony white clumps interspersed with blue sky.