Where the cloud begins

Rising air cools. When it reaches saturation, tiny droplets can form: invisible water vapour becomes a visible cloud. This is why many cumulus clouds have fairly flat bases. Other clouds form differently and have less regular boundaries.

How the height is measured

A ceilometer sends light pulses upwards and analyses the light scattered back. The travel time reveals the height. It measures above its own location; a nearby gap cannot be treated as a measurement of the whole sky.

Cloud base is not always a ceiling

In aviation, a ceiling is the base of the lowest layer covering more than half the sky, or a vertical visibility when the sky is obscured. One isolated low cloud therefore does not automatically create a ceiling.

Above which ground?

A cloud 500 metres above a plain may already touch a hillside. Metres above ground and metres above sea level are different references. Different model methods and multiple cloud layers can also produce different reported values.

Back to Weather Glossary

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