Relative Humidity Calculator
Determine the moisture content in the air based on air temperature and dew point.
What is Relative Humidity?
Relative humidity (RH) is a measure of the current amount of water vapor in the air relative to the maximum amount of water vapor the air can hold at that specific temperature. It is expressed as a percentage. When the relative humidity reaches 100%, the air is saturated, and water vapor begins to condense into liquid water (dew or fog).
How This Calculator Works
This tool uses the Magnus-Tetens Formula to determine the saturation vapor pressure and actual vapor pressure based on your input of ambient air temperature and dew point temperature. The calculation follows these scientific steps:
- Determine the Actual Vapor Pressure using the Dew Point.
- Determine the Saturation Vapor Pressure using the Air Temperature.
- Divide the Actual by the Saturation and multiply by 100.
Formula Used
RH = 100 × (exp((17.625 × Td) / (243.04 + Td)) / exp((17.625 × T) / (243.04 + T)))
Where:
T = Air Temperature in Celsius
Td = Dew Point Temperature in Celsius
Practical Example
Suppose the current air temperature is 25°C and the dew point is 15°C. Using the Magnus formula approximation:
- The saturation vapor pressure at 25°C is approximately 31.67 hPa.
- The actual vapor pressure at a dew point of 15°C is approximately 17.04 hPa.
- Calculation: (17.04 / 31.67) × 100 = 53.8% Relative Humidity.
Importance of Monitoring Humidity
Relative humidity plays a critical role in human comfort, health, and building maintenance. High humidity (>60%) can encourage mold growth and dust mites, while very low humidity (<30%) can cause dry skin, respiratory irritation, and damage to wooden furniture or musical instruments.