Saturation Vapor Pressure Equation:
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Saturation vapor pressure is the pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases at a given temperature. It represents the maximum amount of water vapor that air can hold at a specific temperature.
The calculator uses the saturation vapor pressure equation:
Where:
Explanation: This empirical equation accurately calculates the saturation vapor pressure of water over a wide range of temperatures commonly encountered in meteorological and environmental applications.
Details: Accurate saturation vapor pressure calculation is crucial for meteorological forecasting, humidity measurement, climate studies, and various engineering applications involving air-water systems.
Tips: Enter temperature in degrees Celsius. The calculator will compute the saturation vapor pressure in kilopascals (kPa).
Q1: What is the physical significance of saturation vapor pressure?
A: It indicates the maximum water vapor content air can hold before condensation occurs at a given temperature.
Q2: How does temperature affect saturation vapor pressure?
A: Saturation vapor pressure increases exponentially with temperature - warmer air can hold significantly more moisture.
Q3: What are typical values of saturation vapor pressure?
A: At 0°C: ~0.61 kPa, at 20°C: ~2.34 kPa, at 40°C: ~7.38 kPa. The values approximately double for every 10°C temperature increase.
Q4: Are there limitations to this equation?
A: This equation provides excellent accuracy for temperatures between 0°C and 60°C, which covers most environmental conditions.
Q5: How is this different from actual vapor pressure?
A: Saturation vapor pressure is the maximum possible, while actual vapor pressure is the current amount of water vapor present in the air.