Last edited 30 Jun 2015

Dew point

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Air will generally include moisture in the form of water vapour.

Relative humidity (RH) is a measure of the water vapour density of air compared to the water vapour density for saturated air at the same temperature and pressure (that is, the maximum amount of moisture that air can “hold” at that temperature and pressure). It is expressed as a percentage.

RH = (actual water vapour density / saturation water vapour density) x 100

When air cools, it is less able to “hold” moisture, that is, the saturation water vapour density falls, and so relative humidity rises. When the relative humidity reaches 100%, the air will be saturated. This is described as the ‘dew pointtemperature, or the ‘saturation temperature’. If the air continues to cool, moisture will begin to condense. Where this condensate forms on a surface, it can be described as ‘dew’, hence the term ‘dew point’.

Understanding this phenomena is important in the design and construction of new buildings, and in the assessment of existing buildings, as the formation of condensation can be damaging, can affect comfort and can be a hazard to health.

Surface condensation occurs where water condenses on the exposed internal surfaces of a building, such as ‘cold’ windows.

Interstitial condensation occurs when the dew point temperature is reached within the fabric of the building, either on the surfaces of components that make up the fabric, or sometimes within the components themselves.

Condensation can cause:

Software is available to help calculate dew points, particularly in relation to interstitial condensation, the position of which within the building fabric is crucial if potential problems are to be avoided.

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