National Physical Laboratory

Humidity and temperature

Thermometer leaning

The capacity of a gas (or a space) to hold water depends on its temperature. The higher the temperature, the more water vapour it can contain.

  • normal room temperature - air typically holds about 1 % of water vapour
  • hot - atmosphere has greater capacity to hold water vapour
  • cold - atmosphere has less capacity to hold water vapour

When the air holds the maximum amount of water vapour at a particular temperature it is said to be saturated.

In air this can happen if:

  1. Capacity is reduced by a lowered temperature and amount of water vapour stays consistent
  2. More water vapour is added.

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