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 humidity calculations and atmospheric science.
The calculator uses the water vapor pressure equation:
Where:
Explanation: The equation calculates the actual water vapor pressure by multiplying the saturation vapor pressure (maximum possible at a given temperature) by the relative humidity expressed as a decimal fraction.
Details: Water vapor pressure is essential for understanding humidity levels, predicting weather patterns, designing HVAC systems, and various industrial processes where moisture control is critical.
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 pressure of water vapor that can exist at a given temperature before condensation occurs.
Q2: How is saturation vapor pressure determined?
A: It depends on temperature and can be calculated using various empirical formulas like the August-Roche-Magnus or Tetens equations.
Q3: What units are used for vapor pressure?
A: Pascals (Pa) are commonly used, but other units like mmHg, hPa, or kPa may also be used depending on the context.
Q4: Why is water vapor pressure important in meteorology?
A: It helps determine humidity levels, predict dew point, and understand atmospheric stability and precipitation patterns.
Q5: How does temperature affect water vapor pressure?
A: Higher temperatures increase the saturation vapor pressure, meaning air can hold more moisture at higher temperatures.