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Cloud types: ten genera, three levels

Meteorologists sort clouds into ten genera, each with a Latin name built from a handful of roots: cirro- for what is high and made of ice, alto- for the middle level, strato- for what spreads in a layer, cumulo- for what heaps up, nimbo- for what brings rain. Once you know the roots, a name such as altocumulus or cirrostratus almost reads itself.

This classification, laid down by the World Meteorological Organization in its International Cloud Atlas, rests on two criteria: the height of the cloud base and the cloud's shape. Observers, pilots and forecasters have used it for over a century, and it is still the best way to make sense of the sky.

Diagram of the three cloud levelsHigh level5,000 to 13,000 mCirrusCirrocumulusCirrostratusMiddle level2,000 to 7,000 mAltocumulusAltostratusNimbostratusLow level0 to 2,000 mStratocumulusStratusCumulusCumulonimbusHeights not to scale; temperate regions
The three levels and the genera whose bases lie in them. Cumulonimbus has a low base but grows up to the high level.

Three levels, one base height

The high level starts at about 5,000 m and reaches 13,000 m in temperate latitudes. It holds cirrus, cirrocumulus and cirrostratus: thin, white clouds of ice crystals. The middle level runs from about 2,000 to 7,000 m: altocumulus and altostratus belong there, and nimbostratus, the cloud of steady rain, has its top there. The low level goes from the ground up to 2,000 m, with stratus, stratocumulus and cumulus.

Cumulonimbus and nimbostratus spill beyond their level: their bases are low, while their tops reach the middle level for the one and the tropopause for the other. They are therefore classed by their base and recognised by their thickness. These heights are lower near the poles and higher towards the equator, and lower in winter than in summer.

To judge a cloud's level without instruments, look at its detail. At low levels you can make out hollows, shadows and sharp edges. The higher the cloud, the thinner, whiter and smoother it looks, because its elements appear smaller to the eye.

The ten genera in one table

GenusLevelBase heightAppearanceAssociated weather
CirrusHigh level5,000 to 13,000 mwhite, silky wisps with no shading of their ownfair weather; a warning of change if it thickens into a veil
CirrocumulusHigh level5,000 to 13,000 mbanks of tiny white grains with no grey sidechange possible; short-lived
CirrostratusHigh level5,000 to 13,000 mwhitish, transparent veil with a halooften signals rain or snow within the day
AltocumulusMiddle level2,000 to 7,000 mwhite and grey rounded patches or rolls, in banksoften fair; castellanus: thunderstorm risk
AltostratusMiddle level2,000 to 7,000 mgrey or bluish sheet, sun as if behind frosted glassrain or snow close, especially if the sky lowers
NimbostratusMiddle level0 to 2,000 mdark grey, very thick layer with a blurred basesteady rain or snow lasting hours
StratocumulusLow level0 to 2,000 mlarge grey and white rolls or patches, joined togethergrey, dry sky; drizzle or light rain possible
StratusLow level0 to 2,000 m, often close to the grounduniform grey layer with no features, very low baselow grey sky; drizzle possible
CumulusLow level0 to 2,000 mwhite heaps with domed tops, flat greyish basefair weather; if it grows, showers and storms possible
CumulonimbusLow level0 to 2,000 m (top up to the tropopause)massive tower, dark base, anvil-shaped topthunderstorm, violent showers, hail, lightning, gusts

The ten genera, drawn

Schematic drawing of cirrus: fine white curved wisps across a deep blue skyCirrusSchematic drawing of cirrocumulus: tiny white grains lined up in rows across a deep blue skyCirrocumulusSchematic drawing of cirrostratus: a milky veil in front of the sun, surrounded by a ring of light, the haloCirrostratusSchematic drawing of altocumulus: rows of white rounded patches with grey undersides across a blue skyAltocumulusSchematic drawing of altostratus: a uniform grey sheet with the sun as a pale disc behind frosted glassAltostratusSchematic drawing of nimbostratus: a thick dark grey layer, steady rain in fine streaks and puddles on the groundNimbostratusSchematic drawing of stratocumulus: rows of large rounded grey elements packed close together with a few gaps of blue skyStratocumulusSchematic drawing of stratus: a uniform low grey layer resting on hills, with trails of mistStratusSchematic drawing of cumulus: a white cauliflower-shaped cloud with a flat base in a blue sky, with the sun and a meadowCumulusSchematic drawing of cumulonimbus: a massive tower with an anvil-shaped top, a dark base, a shower and a lightning bolt over a fieldCumulonimbus

How to use this table

Start with the level: look up and ask whether the cloud is high and thin, middle and dappled, or low and bulky. Then look at the shape: filaments, grains, a continuous veil, rounded heaps or a uniform grey layer. The name follows from the two. A thin veil of ice crystals at high level is cirrostratus; a thick grey layer that hides the sun and gives steady rain is nimbostratus.

Often several genera are stacked in the same sky. Observers then record each layer separately, from lowest to highest, with the share of sky it covers in eighths (oktas). The "today" block on each cloud page follows the same idea: it gives the forecast average cover at each level for the country's largest city.

Sources

  • World Meteorological Organization (WMO), International Cloud Atlas, WMO-No. 407: definitions of the genera, levels and base heights for temperate regions. https://cloudatlas.wmo.int (copyright WMO; no text or image from the Atlas is reproduced here).
  • Drawings and text: original to this site.

Other pages of the Atlas

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