Calculate the temperature at which dew forms based on current conditions
The dew point is the temperature to which air must be cooled to become saturated with water vapor. When cooled further, the airborne water vapor will condense to form liquid water (dew). Higher dew points mean more moisture in the air, which makes it feel more humid.
Our calculator uses the August-Roche-Magnus approximation, which provides accurate results for temperatures between -45°C and 60°C (-49°F to 140°F).
The dew point formula we use is:
Td = (b × α(T,RH)) / (a - α(T,RH))
Where α(T,RH) = (a × T / (b + T)) + ln(RH/100)
a = 17.27, b = 237.7°C for Celsius or a = 17.625, b = 243.04°C for Fahrenheit
The dew point is the temperature at which air becomes saturated with moisture and dew begins to form. It's a better measure of humidity than relative humidity because:
When the dew point equals the air temperature, the relative humidity is 100% and fog or dew is likely to form.
Dew point is directly related to how comfortable we feel:
High dew points make it harder for sweat to evaporate, reducing our natural cooling mechanism. This makes temperatures feel much hotter than they actually are.
Dew point calculations are essential for:
In building construction, dew point calculations help prevent moisture damage by ensuring walls and insulation are designed to avoid condensation within the structure.