Water vapour condensed into minute water particles that float in masses in the atmosphere. Clouds, like fogs or mists, that occur at lower levels, are formed by the cooling of air containing water vapour, which generally condenses around tiny dust particles.
Clouds are classified according to the height at which they occur, and by their shape.
Cirrus and
cirrostratus clouds occur at around 10 km/33,000 ft. The former, sometimes called mares'-tails, consist of minute specks of ice and appear as feathery white wisps, while cirrostratus clouds stretch across the sky as a thin white sheet. Three types of cloud are found at 37 km/10,00023,000 ft: cirrocumulus, altocumulus, and altostratus.
Cirrocumulus clouds occur in small or large rounded tufts, sometimes arranged in the pattern called mackerel sky.
Altocumulus clouds are similar, but larger, white clouds, also arranged in lines.
Altostratus clouds are like heavy cirrostratus clouds and may stretch across the sky as a grey sheet.
Stratocumulus clouds are generally lower, occurring at 26 km/6,50020,000 ft. They are dull grey clouds that give rise to a leaden sky that may not yield rain. Two types of clouds,
cumulus and
cumulonimbus, are placed in a special category because they are produced by daily ascending air currents, which take moisture into the cooler regions of the atmosphere. Cumulus clouds have a flat base generally at 1.4 km/4,500 ft where condensation begins, while the upper part is dome-shaped and extends to about 1.8 km/6,000 ft. Cumulonimbus clouds have their base at much the same level, but extend much higher, often up to over 6 km/20,000 ft. Short heavy showers and sometimes thunder may accompany them.
Stratus clouds, occurring below 12.5 km/3,0008,000 ft, have the appearance of sheets parallel to the horizon and are like high-level fogs.
In addition to their essential role in the water cycle, clouds are important in the regulation of radiation in the Earth's atmosphere. They reflect short-wave radiation from the Sun, and absorb and re-emit long-wave radiation from the Earth's surface.
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