Absolute Humidity Formula:
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Definition: Absolute humidity is the measure of water vapor in the air, regardless of temperature, expressed as grams of water vapor per cubic meter of air (g/m³).
Purpose: This calculator determines the actual amount of water vapor present in the air based on dew point and ambient temperature.
The calculator uses the formula:
Where:
Explanation: The formula calculates saturation vapor pressure from dew point, then converts it to absolute humidity using the ideal gas law.
Details: Absolute humidity is crucial for HVAC design, industrial processes, meteorology, and understanding human comfort levels.
Tips: Enter the dew point temperature and ambient temperature in Celsius. Dew point cannot exceed ambient temperature.
Q1: What's the difference between absolute and relative humidity?
A: Absolute humidity measures actual water vapor content, while relative humidity is the percentage of vapor relative to maximum capacity at that temperature.
Q2: Why does dew point matter for absolute humidity?
A: Dew point is the temperature at which air becomes saturated, directly relating to the actual water vapor content.
Q3: What's a typical absolute humidity range?
A: Comfortable indoor air is typically 5-12 g/m³. Below 5 is dry, above 12 feels humid.
Q4: How does temperature affect the calculation?
A: Temperature appears in the denominator to convert vapor pressure to density (g/m³).
Q5: What if my dew point equals ambient temperature?
A: This means 100% relative humidity (air is saturated) and the highest possible absolute humidity for that temperature.