Relative Humidity Formula:
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Relative Humidity (RH) is the ratio of the current absolute humidity to the highest possible absolute humidity at that temperature, expressed as a percentage. It indicates how much water vapor is in the air compared to how much it could hold at that temperature.
The calculator uses the Relative Humidity formula:
Where:
Explanation: The formula compares the actual amount of water vapor in the air (e) to the maximum amount the air can hold at that temperature (es), then converts this ratio to a percentage.
Details: Relative humidity affects human comfort, building design, industrial processes, and weather forecasting. It's crucial for HVAC systems, agriculture, and many manufacturing processes.
Tips: Enter both actual vapor pressure and saturation vapor pressure in kPa (kilopascals). Both values must be positive numbers.
Q1: What's the difference between absolute and relative humidity?
A: Absolute humidity measures actual water vapor content (g/m³), while relative humidity measures this as a percentage of maximum possible at that temperature.
Q2: What are typical RH values?
A: Comfortable indoor RH is typically 30-50%. Below 30% may feel dry, above 60% promotes mold growth.
Q3: How does temperature affect RH?
A: Warmer air can hold more moisture, so RH decreases as temperature rises (if moisture content stays constant).
Q4: How is saturation vapor pressure determined?
A: It's calculated from temperature using the Magnus formula or similar equations.
Q5: Why measure in kPa?
A: kPa is the SI unit for pressure. Some systems may use hPa (1 hPa = 0.1 kPa) or mmHg (1 kPa ≈ 7.5 mmHg).