Relative Humidity Calculator

Calculate relative humidity, dew point, and wet-bulb temperature from dry-bulb temperature and dew point measurement using the Magnus formula.

RELATIVE HUMIDITY
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Sat. Vapor Press. (hPa)
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Actual Vapor Press. (hPa)
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Mixing Ratio (g/kg)
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Wet-Bulb Est. (°C)
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What Is Relative Humidity?

Relative humidity (RH) is the ratio of the current absolute humidity to the maximum possible humidity at the same temperature, expressed as a percentage. When air is saturated (100% RH), it cannot hold any more water vapor, and condensation begins. The relationship between temperature and the air's capacity to hold moisture is described by the Clausius-Clapeyron equation.

Understanding relative humidity is essential in meteorology, HVAC design, agriculture, material preservation, and human comfort. The ideal indoor relative humidity for comfort and health is between 40% and 60%. Values below 30% cause dry skin and respiratory irritation, while values above 70% promote mold growth and dust mites.

Humidity Formulas

e_s(T) = 6.112 × exp(17.67 × T / (T + 243.5)) (Magnus formula)
RH = 100 × e_s(T_dew) / e_s(T_dry)
Mixing Ratio = 621.97 × e / (P - e) g/kg

Comfort Zones

RH RangeComfort LevelHealth Effects
< 25%Very DryDry skin, static electricity, respiratory issues
25-40%DryComfortable for most, minor dryness
40-60%IdealOptimal comfort and health
60-80%HumidFeels muggy, mold risk increases
> 80%Very HumidOppressive, high mold/mildew risk

Effects of Humidity

  • Human comfort: High humidity impairs the body's ability to cool through evaporation, making hot weather feel even hotter.
  • Building damage: Excess moisture causes wood warping, paint peeling, and corrosion of metal components.
  • Electronics: High humidity can cause condensation on circuit boards, leading to short circuits and corrosion.
  • Agriculture: Humidity affects crop diseases, pollination, and transpiration rates in plants.

Frequently Asked Questions

What is dew point and why does it matter?

The dew point is the temperature at which air becomes saturated and condensation begins. It is a direct measure of the actual moisture content in the air. A dew point of 20C feels muggy regardless of the air temperature, while a dew point below 10C feels dry and comfortable. Dew point is more useful than RH for assessing comfort because RH changes with temperature even when moisture stays constant.

Can relative humidity exceed 100%?

In theory, RH cannot exceed 100%. However, in practice, supersaturation can briefly occur (up to about 101-102%) when there are insufficient condensation nuclei. This is uncommon and unstable -- the excess moisture quickly condenses on available surfaces or aerosol particles, forming fog or clouds.

How does temperature affect relative humidity?

Warming air increases its moisture capacity, so RH drops even if the actual moisture stays the same. This is why winter indoor air feels dry -- cold outdoor air with high RH is heated indoors, dramatically lowering the RH. Conversely, cooling air raises RH. This is the principle behind dehumidifiers and air conditioning.