> 100 km altitude

clouds

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The void.txt

> 100 km

Spatium

The void

Above 100 km is the Kármán line, the boundary of outer space. There are no more clouds up here, just the vast dark of the cosmos. The Earth looks impossibly blue from here, wrapped in its thin veil of atmosphere.

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The void.jpg
The void clouds
NASA/Apollo 17 · Public Domain
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Noctilucent clouds.txt

76 – 85 km

Noctilucent / NLC

Noctilucent clouds

Noctilucent clouds glow electric blue-silver after sunset because they're so high up that sunlight still reaches them in the dark. They form near the poles in summer from water vapour freezing around cosmic dust.

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Noctilucent clouds.jpg
Noctilucent clouds clouds
Matthias Süßen · CC BY-SA 4.0
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Cirrostratus.txt

6 – 12 km

Cirrostratus

Cirrostratus

Cirrostratus clouds are translucent sheets of ice crystals so thin you can barely see them, but they create beautiful halos around the sun or moon. If you've ever seen a ring of light around the moon at night, that was thanks to the cirrostratus' refraction and reflection of ice crystals.

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Cirrostratus.jpg
Cirrostratus clouds
Fir0002 · CC BY-SA 3.0
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Cirrus.txt

6 – 12 km

Cirrus

Cirrus

Cirrus clouds are made entirely of ice crystals, which is why they look like wispy brushstrokes. Temperatures here drop to -40°C.

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Cirrus.jpg
Cirrus clouds
Fir0002 · CC BY-SA 3.0
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Altostratus.txt

2 – 7 km

Altostratus

Altostratus

Altostratus is a grey-blue veil stretched across the sky, thin enough to show the sun as a blurry disc. They often bring steady rain or snow within 12 to 24 hours.

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Altostratus.jpg
Altostratus clouds
PiccoloNameki · CC BY-SA 3.0
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Altocumulus.txt

2 – 7 km

Altocumulus

Altocumulus

Altocumulus are the mid-level clouds that look like a sky full of cotton balls or fish scales—this pattern is called a 'mackerel sky'. They often appear before a warm front.

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Altocumulus.jpg
Altocumulus clouds
LivingShadow · CC BY-SA 3.0
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Cumulus.txt

500 m – 2 km

Cumulus

Cumulus

Cumulus clouds are the archetypal cloud! They form when warm air rises and cools, puffing up into those beautiful cauliflower towers. A sunny day with fair-weather cumulus is basically peak meteorological contentment. These clouds rarely rain, but they can produce light showers if they grow vertically in size.

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Cumulus.jpg
Cumulus clouds
Fir0002 · CC BY-NC 3.0
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Stratocumulus.txt

500 m – 2 km

Stratocumulus

Stratocumulus

Stratocumulus clouds are the most common cloud on the planet. They cover about 23% of the Earth's surface at any given moment. They're lumpy, patchy, and often look like someone dragged a comb through a grey sky.

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Stratocumulus.jpg
Stratocumulus clouds
William Crochot · CC BY-SA 4.0
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Stratus.txt

100 m – 2 km

Stratus

Stratus

Stratus clouds are low-level clouds that blanket the sky. They cover the whole sky in a flat, uniform sheet and rarely produce more than a light drizzle of rain.

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Stratus.jpg
Stratus clouds
Couch-scratching-cats · CC BY 2.5
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Fog.txt

0 – 100 m

Nebula

Fog

Fog is essentially a low-lying cloud that touches the ground or gets close to it. In aviation, fog is defined specifically as a cloud whose base within 15m (50ft) of the ground. Fog forms when air cools to its dew point, suspending tiny little water droplets in the air. If visibility is less than 1km, it's considered fog; if visibility is greater than 1km, it's mist.

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Fog.jpg
Fog clouds
Bernhard Hanakam · CC BY-SA 3.0