Virtual Temperature Equation:
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Virtual temperature (Tv) is the temperature that dry air would have if its pressure and density were equal to those of a given sample of moist air. It accounts for the effect of water vapor on air density.
The calculator uses the virtual temperature equation:
Where:
Explanation: The equation adjusts the actual temperature to account for the reduced density of moist air compared to dry air at the same temperature and pressure.
Details: Virtual temperature is crucial in meteorology for accurate calculations of air density, which affects atmospheric dynamics, buoyancy, and weather forecasting models.
Tips: Enter temperature in Kelvin, vapor pressure in Pascals, and total pressure in Pascals. All values must be valid (temperature > 0, pressure > 0, vapor pressure ≥ 0).
Q1: Why is virtual temperature higher than actual temperature?
A: Moist air is less dense than dry air at the same temperature and pressure, so virtual temperature represents the higher temperature dry air would need to have the same density.
Q2: When is virtual temperature most significant?
A: The difference is most significant in warm, humid conditions where water vapor content is high.
Q3: What units should be used for input?
A: The calculator uses Kelvin for temperature and Pascals for pressure. Convert from Celsius by adding 273.15 to °C.
Q4: What is a typical range for virtual temperature?
A: In Earth's atmosphere, virtual temperature is typically 1-3% higher than actual temperature, but can be more in very humid conditions.
Q5: How does this relate to potential temperature?
A: Virtual potential temperature can be calculated similarly to potential temperature but using virtual temperature instead of actual temperature.