Relative Humidity Formula:
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Relative Humidity (RH) 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. It's a key parameter in meteorology, HVAC, and many industrial processes.
The calculator uses the RH formula:
Where:
Explanation: The equation calculates what percentage the actual vapor pressure is of the saturation vapor pressure at the same temperature.
Details: Relative humidity affects human comfort, building design, industrial processes, and is crucial for weather forecasting and climate studies.
Tips: Enter both vapor pressure values in kPa. Both values must be positive numbers, and the actual vapor pressure cannot exceed the saturation vapor pressure.
Q1: What's the difference between RH and absolute humidity?
A: RH is relative to temperature (percentage), while absolute humidity measures the actual water content (g/m³) regardless of temperature.
Q2: What are comfortable RH levels for humans?
A: Typically 30-60%. Below 30% can cause dryness, above 60% promotes mold growth and feels uncomfortable.
Q3: How does temperature affect RH?
A: Warmer air can hold more moisture, so RH changes with temperature even if the actual water content stays the same.
Q4: How is saturation vapor pressure determined?
A: It's calculated from temperature using the Clausius-Clapeyron equation or looked up in thermodynamic tables.
Q5: Why use kPa for vapor pressure?
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).