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Condensation and mould

Condensation forms wherever a surface is colder than the dew point of the room air. Lower the humidity or warm the surface and it stops.

At 20 °C and 60 % RH
Dew point about 12 °C
Detailed view of water droplets on a glass window with a blue background
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Warm air holds more water vapour than cold air. When room air touches a cold window or an outside wall, it cools, and if the surface is below the dew point water condenses on it. Repeated condensation is what feeds black mould.

Use the dew point calculator to see how cold a surface has to be before it gets wet, and the humidity you need to keep it dry.

Persistent damp patches, tide marks or damp that does not follow the weather can have other causes such as leaks or penetrating damp. A dehumidifier treats the air, not the building.

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