Water Vapor Pressure Equation:
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Water vapor pressure is the partial pressure of water vapor in any gas mixture. It represents the contribution of water vapor to the total pressure and is a key parameter in atmospheric science, meteorology, and various engineering applications.
The calculator uses the water vapor pressure equation:
Where:
Explanation: The equation calculates the actual vapor pressure from relative humidity and the saturation vapor pressure at the same temperature.
Details: Accurate water vapor pressure calculation is crucial for weather forecasting, HVAC system design, industrial processes, and understanding various atmospheric phenomena.
Tips: Enter relative humidity as a percentage (0-100%) and saturation vapor pressure in Pascals (Pa). Both values must be valid positive numbers.
Q1: What is saturation vapor pressure?
A: Saturation vapor pressure is the maximum vapor pressure that can exist at a given temperature, when the air is saturated with water vapor.
Q2: How does temperature affect water vapor pressure?
A: Saturation vapor pressure increases exponentially with temperature, meaning warmer air can hold more water vapor.
Q3: What units are typically used for vapor pressure?
A: Vapor pressure is commonly measured in Pascals (Pa), but may also be expressed in millibars (mb) or millimeters of mercury (mmHg).
Q4: Why is water vapor pressure important in meteorology?
A: It's essential for calculating humidity parameters, predicting dew point, and understanding cloud formation and precipitation processes.
Q5: How is saturation vapor pressure calculated?
A: Saturation vapor pressure can be calculated using various empirical formulas, most commonly the Magnus formula or the Goff-Gratch equation.