Vapor Pressure Equation:
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Vapor pressure is the pressure exerted by water vapor in thermodynamic equilibrium with its condensed phases at a given temperature. It represents the tendency of water molecules to escape from the liquid phase into the gas phase.
The calculator uses the vapor pressure equation:
Where:
Explanation: This empirical equation accurately calculates the saturation vapor pressure of water over a wide range of temperatures, based on the Magnus formula.
Details: Vapor pressure calculations are essential in meteorology, HVAC design, industrial processes, and environmental science for understanding humidity, evaporation rates, and phase change phenomena.
Tips: Enter temperature in degrees Celsius. The calculator will compute the saturation vapor pressure of water at that temperature in kilopascals.
Q1: What is the range of validity for this equation?
A: This equation provides accurate results for temperatures between -50°C and 100°C, covering most practical applications.
Q2: How does vapor pressure change with temperature?
A: Vapor pressure increases exponentially with temperature - doubling approximately every 10°C increase in temperature.
Q3: Why is vapor pressure important in weather forecasting?
A: Vapor pressure helps determine humidity levels, dew point, and the likelihood of precipitation, making it crucial for weather prediction.
Q4: How does altitude affect vapor pressure?
A: While the saturation vapor pressure at a given temperature remains constant regardless of altitude, the actual vapor pressure in the atmosphere decreases with altitude due to lower atmospheric pressure.
Q5: What's the difference between vapor pressure and partial pressure?
A: Vapor pressure specifically refers to the pressure exerted by a vapor in equilibrium with its liquid phase, while partial pressure is the pressure that a gas would exert if it alone occupied the entire volume.