Absolute Humidity Equation:
From: | To: |
Absolute humidity is the measure of water vapor (moisture) in the air, regardless of temperature. It is expressed as grams of water vapor per cubic meter of air (g/m³). Unlike relative humidity, absolute humidity does not fluctuate with changes in temperature or pressure.
The calculator uses the absolute humidity equation:
Where:
Explanation: This equation calculates the actual amount of water vapor present in the air by combining relative humidity with temperature-dependent saturation vapor pressure.
Details: Absolute humidity is important in meteorology, HVAC design, industrial processes, and health applications. It provides a more accurate measure of moisture content than relative humidity for many scientific and engineering applications.
Tips: Enter relative humidity as a percentage (0-100), saturation vapor pressure in Pascals, gas constant for water vapor (default is 461.5 J/kg·K), and temperature in Kelvin. All values must be positive numbers.
Q1: What's the difference between absolute and relative humidity?
A: Absolute humidity measures the actual amount of water vapor in the air, while relative humidity expresses how close the air is to saturation at its current temperature.
Q2: Why use Kelvin for temperature?
A: Kelvin is an absolute temperature scale required for thermodynamic calculations involving gas constants.
Q3: How do I find saturation vapor pressure?
A: SVP can be calculated using various equations (like Magnus formula) or obtained from standard meteorological tables based on temperature.
Q4: What are typical absolute humidity values?
A: Values range from near 0 g/m³ in arid conditions to about 30 g/m³ in very humid tropical environments.
Q5: Can I use this calculator for any altitude?
A: The calculation is valid at any altitude as long as proper values for SVP are used (which varies with pressure).