Absolute Humidity Equation:
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Absolute Humidity (AH) is the measure of water vapor in the air, regardless of temperature. It's expressed as the mass of water vapor per unit volume of air (kg/m³). Unlike relative humidity, absolute humidity isn't affected by temperature changes.
The calculator uses the absolute humidity equation:
Where:
Explanation: The equation calculates the actual amount of water vapor present in the air by relating vapor pressure to temperature through fundamental physical constants.
Details: Absolute humidity is crucial in meteorology, HVAC design, industrial processes, and health applications. It directly affects evaporation rates, human comfort, and many industrial processes.
Tips: Enter vapor pressure in Pascals (Pa) and temperature in Kelvin (K). Both values must be positive numbers. For accurate results, use precise measurements of vapor pressure and temperature.
Q1: How is absolute humidity different from relative humidity?
A: Absolute humidity measures the actual water vapor content, while relative humidity measures how close the air is to saturation at its current temperature.
Q2: What are typical absolute humidity values?
A: Near sea level, absolute humidity typically ranges from near 0 to about 30 g/m³ (0.03 kg/m³) in very humid conditions.
Q3: How do I convert relative humidity to vapor pressure?
A: First calculate saturation vapor pressure using the Clausius-Clapeyron equation, then multiply by relative humidity (as a decimal).
Q4: Why use Kelvin for temperature?
A: The gas constant R is defined using Kelvin, and using absolute temperature prevents division by zero in calculations.
Q5: What's the relationship between absolute humidity and dew point?
A: Dew point is the temperature at which air becomes saturated with the current absolute humidity, causing condensation.