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 amount the air can hold at that temperature, expressed as a percentage. It indicates how close the air is to saturation.
The calculator uses the Relative Humidity formula:
Where:
Explanation: The formula calculates the percentage of moisture in the air relative to the maximum moisture capacity at the same temperature.
Details: Relative humidity is crucial for weather forecasting, climate studies, agricultural planning, industrial processes, and maintaining comfortable indoor environments. It affects human comfort, health, and various material properties.
Tips: Enter specific humidity and saturation specific humidity values in kg/kg. Both values must be positive, and SH should not exceed SH_sat for valid results.
Q1: What's the difference between specific and relative humidity?
A: Specific humidity measures the actual mass of water vapor per mass of air, while relative humidity expresses this as a percentage of the maximum possible at that temperature.
Q2: What are typical relative humidity ranges?
A: Comfortable indoor RH is typically 30-50%. Below 30% can cause dryness, above 60% can promote mold growth and feel uncomfortable.
Q3: How does temperature affect relative humidity?
A: Warmer air can hold more moisture, so relative humidity decreases as temperature rises (if moisture content remains constant), and vice versa.
Q4: Why can't specific humidity exceed saturation specific humidity?
A: Saturation specific humidity represents the maximum water vapor air can hold at a given temperature. Exceeding this would result in condensation.
Q5: How is relative humidity measured in practice?
A: Typically using hygrometers, psychrometers, or electronic sensors that measure various properties affected by moisture content.