Relative Humidity Equation:
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Relative Humidity (RH) is the ratio of the current absolute humidity to the highest possible absolute humidity at that air temperature, expressed as a percentage. It indicates how much water vapor is in the air compared to how much the air can hold at that temperature.
The calculator uses the Relative Humidity equation:
Where:
Explanation: The equation calculates what percentage the actual water vapor pressure is of the saturation vapor pressure at the same temperature.
Details: Relative humidity affects human comfort, health, building construction, and various industrial processes. It's crucial for weather forecasting, agriculture, and HVAC system design.
Tips: Enter both actual vapor pressure (e) and saturation vapor pressure (es) in kPa. Both values must be positive numbers.
Q1: What's the difference between absolute and relative humidity?
A: Absolute humidity measures the actual amount of water vapor in the air (g/m³), while relative humidity measures how close the air is to saturation (%).
Q2: What are typical comfortable RH levels?
A: For human comfort, 30-50% RH is generally recommended. Below 30% may feel too dry, above 60% may feel muggy.
Q3: How does temperature affect RH?
A: Warmer air can hold more moisture, so RH changes with temperature even if the actual moisture content stays the same.
Q4: Why does RH matter in buildings?
A: High RH can promote mold growth, while low RH can cause dry skin and respiratory irritation.
Q5: How is saturation vapor pressure determined?
A: It's calculated from temperature using the Clausius-Clapeyron equation or looked up in thermodynamic tables.