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Glossary · Environment and light

Dew point

Dew point is the temperature at which air becomes saturated and water starts condensing; when leaves or buds cool to it, free water forms and mould risk jumps.

Also written dewpointdew-point temperatureTdcondensation point

EstablishedDraft: awaiting expert reviewUpdated

The dew point is the temperature to which air must be cooled, at constant water content, to reach 100% relative humidity. Any surface at or below the dew point collects condensation. Because it depends only on how much water the air holds, it is a more stable measure of moisture than RH.

In practice

Air at 26 °C (79 °F) and 60% RH has a dew point of about 17.6 °C (64 °F). If lights go off and the room or the inside of a dense cola drops to that temperature, water condenses on tissue. Leaves radiating heat to a cool ceiling or wall can sit a degree or two below air temperature, so trouble can start even when the air itself is above the dew point.

Rule of thumb for flower: keep the coldest surface in the canopy at least 3–5 °C (5–9 °F) above the dew point, especially in the first hour after lights-off. Run dehumidification and airflow through the dark period and ramp temperature down slowly. Free water on buds for a few hours is enough for botrytis spores to germinate.

Units and formula

Magnus approximation (°C): Td = 243.04 × γ ÷ (17.625 − γ), where γ = ln(RH ÷ 100) + 17.625 × T ÷ (243.04 + T).

Don't confuse with

  • Relative humidity: changes with temperature; dew point does not.
  • Frost point: the equivalent below 0 °C, where ice forms.

Related terms

Sources

  1. Allen RG, Pereira LS, Raes D, Smith M, 1998. Crop evapotranspiration: guidelines for computing crop water requirements (FAO Irrigation and Drainage Paper 56), Chapter 3. FAO. fao.org/4/x0490e/x0490e07.htm
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