Formula Used:
| From: | To: |
The saturation pressure of water vapor is the maximum partial pressure that water vapor can have in air at a given temperature without condensing. It represents the pressure at which air becomes fully saturated with water vapor.
The calculator uses the formula:
Where:
Explanation: This formula calculates the saturation pressure by dividing the actual water vapor pressure by the relative humidity, which represents the ratio of actual vapor pressure to saturation vapor pressure.
Details: Calculating saturation pressure is crucial for understanding atmospheric conditions, predicting weather patterns, designing HVAC systems, and studying evaporation and condensation processes in various industrial applications.
Tips: Enter water vapor pressure in Pascal, relative humidity as a value between 0 and 1. Both values must be positive, with relative humidity not exceeding 1.
Q1: What is the relationship between saturation pressure and temperature?
A: Saturation pressure increases exponentially with temperature. Warmer air can hold more water vapor before becoming saturated.
Q2: How does relative humidity affect saturation pressure calculations?
A: Relative humidity is the ratio of actual vapor pressure to saturation vapor pressure, so knowing both allows calculation of the saturation pressure.
Q3: What are typical values for water vapor saturation pressure?
A: At room temperature (20°C), saturation pressure is about 2330 Pascal. At 100°C (boiling point), it's 101325 Pascal (1 atmosphere).
Q4: Why is saturation pressure important in meteorology?
A: It helps predict dew point, fog formation, and precipitation. When actual vapor pressure reaches saturation pressure, condensation occurs.
Q5: How does altitude affect saturation pressure calculations?
A: Saturation pressure depends primarily on temperature, not altitude. However, atmospheric pressure decreases with altitude, affecting the partial pressures of all gases.