Relative Humidity Formula:
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Definition: Relative humidity is the ratio of the current amount of water vapor in the air to the maximum possible amount at that temperature, expressed as a percentage.
Purpose: RH is crucial for weather forecasting, HVAC systems, industrial processes, and maintaining comfortable indoor environments.
The calculator uses the formula:
Where:
Explanation: The actual vapor pressure is divided by the saturation vapor pressure and multiplied by 100 to get a percentage.
Details: Proper RH levels affect human comfort, prevent mold growth, preserve materials, and are critical in many industrial and agricultural processes.
Tips: Enter both vapor pressures in Pascals (Pa). The saturation pressure must be ≥ actual vapor pressure. Typical values range from 600 Pa to 3000 Pa depending on temperature.
Q1: How do I find vapor pressure values?
A: Use psychrometric charts, equations like Magnus formula, or measure with hygrometers and convert to vapor pressure.
Q2: What's a comfortable RH range for humans?
A: Typically 30-60%. Below 30% can cause dryness, above 60% promotes mold growth.
Q3: Does temperature affect RH?
A: Yes, since saturation vapor pressure (eₛ) changes with temperature while actual vapor pressure (e) may remain constant.
Q4: What's the relationship between dew point and RH?
A: Dew point is the temperature at which RH would be 100%. Higher dew points indicate more moisture in the air.
Q5: Why does RH change throughout the day?
A: RH varies inversely with temperature when moisture content is constant - higher in cool mornings, lower in warm afternoons.