Saturday, October 15, 2016

Clouds and Cloud Types

Clouds are a collection of water droplets or ice crystals. The warmer the air temperature, the more water vapour (gas) that the air can hold. However, when the air starts to cool, water vapour starts to condense as long as it has condensation nuclei to condense around.

Cirrus


Cirrus Clouds
  • Found high in the atmosphere – usually over 5,500 metres
  • Common throughout the world
  • Thin and wispy in appearance
  • Move fairly quickly

Stratus 


Stratus Clouds
  • Low level – below 2000m and sometimes reaching ground.
  • Usually grey and colour and move fast.
  • Can produce light rain and snow

Cumulonimbus


Cumulonimbus Clouds
  • Large clouds up to 10km high and across.
  • They resemble giant cauliflower.
  • Produce rain, thunder and lightening
  • Usually found in spring and summer

Cumulus


Cumulus Clouds
  • Fairly low clouds with bottom between 600m and 1200m
  • Look like lumps of cotton wool
  • Can produce light rain
  • Individual clouds have a short life cycle

See the following video on Cloud Types


There are ten main types of which can be split into three categories according to height.

Look at this diagram, you can see the sub divisions of the clouds.

Cloud Types
High clouds are between 5500 and 14000 m above the ground, they are usually composed solely of ice crystals;
Medium clouds, between 2000m and 7000m are usually composed of water droplets or a mixture of ice crystals and water droplets:
Low clouds below 2000m, usually made up of water droplets;
  • stratocumulus - layered series of rounded rolls, generally white;
  • stratus - layered uniform grey
  • cumulus - 'white cauliflower' clouds with flat base;
  • cumulonimbus - large dark towers, often with 'anvil' tops, associated with heavy rain and thunderstorms


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