Relative Humidity Equation:
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Relative Humidity (RH) is a measure of the amount of water vapor in the air compared to the maximum amount the air can hold at that temperature. It's expressed as a percentage and is calculated using vapor pressures at wet and dry bulb temperatures.
The calculator uses the Relative Humidity equation:
Where:
Explanation: The equation calculates the ratio of actual water vapor pressure to saturation vapor pressure, multiplied by 100 to get a percentage.
Details: Relative humidity is crucial for weather forecasting, HVAC system design, industrial processes, and maintaining comfortable and healthy indoor environments.
Tips: Enter vapor pressures in Pascals (Pa) for both wet and dry bulb measurements. Both values must be positive numbers.
Q1: What's the difference between RH and absolute humidity?
A: RH is a percentage of moisture relative to capacity, while absolute humidity is the actual mass of water vapor per volume of air.
Q2: What are typical RH ranges for comfort?
A: 30-50% RH is generally comfortable for humans. Below 30% may feel dry, above 60% may feel muggy.
Q3: How do I measure e_w and e_d?
A: Use a psychrometer (wet-dry bulb thermometer) and convert temperatures to vapor pressures using standard tables or equations.
Q4: Why does RH change with temperature?
A: Warmer air can hold more moisture, so RH decreases as temperature rises (if moisture content stays constant).
Q5: What instruments measure RH directly?
A: Hygrometers and modern electronic sensors can measure RH directly without needing separate wet/dry measurements.