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 grams of water vapor per kilogram of dry air (g/kg). Unlike relative humidity, absolute humidity isn't affected by temperature changes.
The calculator uses the absolute humidity equation:
Where:
Explanation: The equation converts relative humidity to absolute humidity by accounting for the maximum possible water vapor (saturation vapor pressure) at the given temperature.
Details: Absolute humidity is crucial for meteorological studies, HVAC system design, industrial processes, and understanding human comfort levels. It provides an absolute measure of moisture content unlike relative humidity which is temperature-dependent.
Tips: Enter relative humidity as percentage (0-100%), saturation vapor pressure in Pascals (Pa), and temperature in Kelvin (K). All values must be positive numbers.
Q1: How is absolute humidity different from 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: What are typical absolute humidity values?
A: Near sea level, absolute humidity ranges from near 0 g/kg in cold dry air to about 30 g/kg in hot humid conditions.
Q3: How do I get saturation vapor pressure?
A: Saturation vapor pressure can be calculated from temperature using the August-Roche-Magnus approximation or looked up in thermodynamic tables.
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. Remember 0°C = 273.15K.
Q5: Can I use this for high-altitude calculations?
A: This equation works at any altitude as long as proper pressure values are used, though air density effects might need consideration for very high altitudes.