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Calculate Water Vapor Pressure From Relative Humidity

Water Vapor Pressure Equation:

\[ e = \frac{RH}{100} \times e_s \]

%
Pa

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1. What is Water Vapor Pressure?

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.

2. How Does the Calculator Work?

The calculator uses the water vapor pressure equation:

\[ e = \frac{RH}{100} \times e_s \]

Where:

Explanation: The equation calculates the actual vapor pressure from relative humidity and the saturation vapor pressure at the same temperature.

3. Importance of Water Vapor Pressure Calculation

Details: Accurate water vapor pressure calculation is crucial for weather forecasting, HVAC system design, industrial processes, and understanding various atmospheric phenomena.

4. Using the Calculator

Tips: Enter relative humidity as a percentage (0-100%) and saturation vapor pressure in Pascals (Pa). Both values must be valid positive numbers.

5. Frequently Asked Questions (FAQ)

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.

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