Water on the Earth evaporates (turns into an invisible gas) and rises up into the sky. Higher up where the air is colder, the water condenses: it changes from a gas to drops of water or crystals of ice. We see these drops of water as clouds. The drops fall back down to earth as rain, and then the water evaporates again. This is called the "water cycle".
Warm air holds more water vapor than cool air. So if warm air with lots of water inside cools, it can form a cloud. These are ways air can cool enough to form clouds:
- when air close to the ground is heated by the sun and rises to where the air is colder.
- along weather fronts warmer air is cooled as it runs into colder air;
- when air goes up the side of a mountain it cools as it goes higher;
- when warm air goes over something colder such as cool water in a lake) or ground that is cooled at night it cools.
Clouds are heavy. The water in a cloud can have a mass of several million tons. Every cubic metre (m3) of the cloud has only about 5 grams of water in it. Cloud droplets are also about 1000 times heavier than evaporated water, so they are much heavier than air. They do not fall, but stay in the air, because there is warm air all round the heavier water droplets. When water changes from gas to droplets, this makes heat. Because the droplets are very small, they "stick" to the warm air.
Sometimes, clouds appear to be brilliant colors at sunrise or sunset. This is due to dust particles in the air.
Cloud classification[change | change source]
Clouds are classified according to how they look and how high the base of the cloud is in the sky. This system was suggested in 1803. There are different sorts of clouds because the air where they form can be still or moving forward or up and down at different speeds. Very thick clouds with large enough water droplets can make rain or snow, and the biggest clouds can make thunder and lightning.
There are five basic families of clouds based on how they look:
- Cirrus clouds are high and thin. The air is very cold at high levels, so these clouds are made of ice crystals instead of water droplets. Cirrus clouds are sometimes called mares' tails because they look like the tails of a horse.
- Stratus clouds are like flat sheets. They may be low-level clouds (stratus), medium-level (altostratus), high-level (cirrostratus), or thick multi-level clouds that make rain or snow (nimbostratus).
- Stratocumulus clouds are in the form of rolls or ripples. They may be low-level clouds (stratocumulus), medium-level (altocumulus), or high-level (cirrocumulus).
- Cumulus clouds are puffly and small when they first form. They may grow into heap clouds that have moderate vertical extent (nothing added to the name), or become towering vertical clouds (towering cumulus).
- Cumulonimbus clouds are very large cumulus-type clouds that usually develop cirrus tops and sometimes other features that give them their own unique look.
The following is a summary of the main cloud types arranged by how high they form:
High-Level clouds[change | change source]
High clouds form from 10,000 to 25,000 ft (3,000 to 8,000 m) in cold places, 16,500 to 40,000 ft (5,000 to 12,000 m) in mild regions and 20,000 to 60,000 ft (6,000 to 18,000 m) in the very hot tropics. They are too high and thin to produce rain or snow.
High-level clouds include:
- Cirrus (Ci)
- Cirrocumulus (Cc)
- Cirrostratus (Cs)
Medium-level clouds[change | change source]
Middle clouds usually form at 6,500 ft (2,000 m) in colder areas. However, they may form as high as 25,000 ft (8,000 m) in the tropics where it's very warm all year. Middle clouds are usually made of water droplets but may also have some ice crystals. They occasionally produce rain or snow that usually evaporates before reaching the ground.
Medium-level clouds include:
- Altocumulus (Ac)
- Altostratus (As)
Low-level clouds[change | change source]
Low-level clouds are usually seen from near ground level to as high as 6,500 ft (2,000 m). Low clouds are usually made of water droplets and may occasionally produce very light rain, drizzle, or snow.
Low-level clouds include:
- Stratocumulus (Sc)
- Stratus (St)
When very low stratus cloud touches the ground, it is called fog.
Moderate-vertical clouds[change | change source]
These are clouds of medium thickness that can form anywhere from near ground level to as high as 10,000 ft (3,000 m). Medium-level cumulus does not have alto added to its name. The tops of these clouds are usually not much higher than 20,000 ft (6,000 m). Vertical clouds often create rain and snow. They are made mostly of water droplets, but when they push up through cold higher levels they may also have ice crystals.
Moderate-vertical clouds include:
- Cumulus (Cu)
- Nimbostratus (Ns)
Towering-vertical clouds[change | change source]
These clouds are very tall with tops usually higher than 20,000 ft (6,000 m). They can create heavy rain and snow showers. Cumulonimbus, the biggest clouds of all, can also produce thunderstorms. These clouds are mostly made of water droplets, but the tops of very large cumulonimbus clouds are often made mostly of ice crystals.
Towering-vertical clouds include:
- Towering cumulus (Tcu)
- Cumulonimbus (Cb)
Gallery[change | change source]
Mountain peaks poking through ragged stratus clouds in the Swiss Alps.
Cumulus cloud bow above the Pacific Ocean with low stratocumulus in the background.
As a sign[change | change source]
References[change | change source]
- Oard, Michael (1997). The Weather Book. P.O. Box 126, Green Forest, AR 72638: Master Books. ISBN 0-89051-211-6.
- E.C. Barrett and C.K. Grant (1976). "The identification of cloud types in LANDSAT MSS images". NASA. http://ntrs.nasa.gov/search.jsp?R=19760014556. Retrieved 22 August 2012.
- "NWS JetStream MAX - The Structure of the Ionosphere". srh.weather.gov. http://www.srh.weather.gov/srh/jetstream/synoptic/clouds_max.htm. Retrieved 22 April 2010.
- "Plymouth State Meteorology Program Cloud Boutique". vortex.plymouth.edu. http://vortex.plymouth.edu/clouds.html/. Retrieved 22 April 2010.
Other websites[change | change source]
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- "BadMeteorology's explanation of why clouds form". ems.psu.edu. http://www.ems.psu.edu/~fraser/Bad/BadClouds.html. Retrieved 22 April 2010.
- "Photographs and information about clouds". chitambo.com. http://www.chitambo.com/clouds/. Retrieved 22 April 2010.
- "Cloud Fraction : Global Maps". earthobservatory.nasa.gov. http://earthobservatory.nasa.gov/GlobalMaps/view.php?d1=MODAL2_M_CLD_FR#. Retrieved 22 April 2010.