Absolute Humidity Equation:
From: | To: |
Absolute Humidity (AH) measures the actual amount of water vapor in the air, expressed as grams of water vapor per kilogram of dry air (g/kg). Unlike relative humidity, it doesn't depend on temperature.
The calculator uses the absolute humidity equation:
Where:
Explanation: The equation converts relative humidity to absolute humidity using the relationship between water vapor pressure and temperature.
Details: Absolute humidity is crucial for meteorological studies, HVAC system design, industrial processes, and understanding human comfort levels.
Tips: Enter relative humidity as percentage, saturation vapor pressure in Pascals, and temperature in Kelvin. All values must be positive numbers.
Q1: What's the difference between absolute and relative humidity?
A: Absolute humidity measures actual water vapor content, while relative humidity measures how close the air is to saturation at its current temperature.
Q2: How do I find saturation vapor pressure?
A: Saturation vapor pressure can be calculated using the Antoine equation or looked up in thermodynamic tables based on temperature.
Q3: What are typical absolute humidity values?
A: Near sea level, absolute humidity typically ranges from 0 g/kg in dry deserts to about 30 g/kg in very humid tropical conditions.
Q4: Why use Kelvin for temperature?
A: Kelvin is used because it's the absolute temperature scale required by the gas law in the equation.
Q5: Can I use this for any altitude?
A: The calculation is valid for any altitude, but saturation vapor pressure decreases with altitude due to lower atmospheric pressure.