Absolute Humidity Equation:
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Absolute humidity (AH) is the actual amount of water vapor in the air, measured in grams of water per cubic meter of air (g/m³). Unlike relative humidity, it doesn't depend on temperature, making it a more precise measurement of moisture content.
The calculator uses the absolute humidity equation:
Where:
Explanation: The equation converts relative humidity to absolute humidity by accounting for temperature-dependent saturation vapor pressure and fundamental physical constants.
Details: Absolute humidity is crucial for meteorological studies, HVAC system design, industrial processes, and understanding human comfort levels. It directly affects evaporation rates and heat transfer.
Tips: Enter relative humidity (0-100%) and temperature in °C. The calculator will output absolute humidity in g/m³. Temperature must be above -273.15°C (absolute zero).
Q1: What's the difference between absolute and relative humidity?
A: Absolute humidity measures actual water vapor content, while relative humidity measures how saturated the air is relative to its maximum capacity at that temperature.
Q2: Why is absolute humidity typically measured in g/m³?
A: Grams per cubic meter provides intuitive understanding of water content, though the SI unit is kg/m³ (1 kg/m³ = 1000 g/m³).
Q3: How does temperature affect absolute humidity?
A: Absolute humidity can remain constant as temperature changes, unlike relative humidity which varies significantly with temperature.
Q4: What are typical absolute humidity values?
A: Comfortable indoor range is 6-12 g/m³. Below 5 g/m³ feels dry, above 15 g/m³ feels muggy. Maximum possible depends on temperature.
Q5: When is absolute humidity more useful than relative humidity?
A: For scientific applications, material drying processes, and when comparing moisture content across different temperatures.