Specific Humidity Formula:
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Specific humidity is defined as the mass of water vapor per unit mass of moist air. It is typically expressed in grams of water vapor per kilogram of air (g/kg). Unlike relative humidity, specific humidity is not temperature-dependent, making it a more precise measure of the actual moisture content in air.
The calculator uses the specific humidity formula:
Where:
Explanation: The formula calculates the mass mixing ratio of water vapor to dry air, then converts it to grams per kilogram.
Details: Specific humidity is crucial in meteorology, climate studies, and HVAC applications. It helps in weather forecasting, understanding atmospheric processes, and designing climate control systems.
Tips: Enter water vapor pressure and total air pressure in Pascals (Pa). Both values must be positive, and total pressure must be greater than water vapor pressure.
Q1: What's the difference between specific humidity and relative humidity?
A: Specific humidity measures the actual moisture content (g/kg), while relative humidity expresses how close the air is to saturation at a given temperature (%).
Q2: Why use Pascals as the pressure unit?
A: Pascals are the SI unit for pressure. The formula works with any consistent pressure units, but inputs must be in the same units.
Q3: What are typical specific humidity values?
A: Values range from near 0 g/kg in dry deserts to about 20 g/kg in very humid tropical regions.
Q4: Can I use hPa instead of Pa?
A: Yes, but ensure both pressure values use the same units (1 hPa = 100 Pa).
Q5: Why is the constant 0.622 used?
A: It represents the ratio of the molecular weight of water vapor (18.015 g/mol) to that of dry air (28.965 g/mol).