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Absolute Humidity Calculator g/kg

Absolute Humidity Equation:

\[ AH = \frac{RH}{100} \times \frac{P_{sat}}{R_v T} \times 1000 \]

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1. What is Absolute Humidity?

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.

2. How Does the Calculator Work?

The calculator uses the absolute humidity equation:

\[ AH = \frac{RH}{100} \times \frac{P_{sat}}{R_v T} \times 1000 \]

Where:

Explanation: The equation converts relative humidity to absolute humidity using the relationship between water vapor pressure and temperature.

3. Importance of Absolute Humidity

Details: Absolute humidity is crucial for meteorological studies, HVAC system design, industrial processes, and understanding human comfort levels.

4. Using the Calculator

Tips: Enter relative humidity as percentage, saturation vapor pressure in Pascals, and temperature in Kelvin. All values must be positive numbers.

5. Frequently Asked Questions (FAQ)

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.

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