Water Vapor Partial Pressure Equation:
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Water vapor partial pressure (e) is the pressure exerted by water vapor in a mixture of gases. It's a key parameter in meteorology, HVAC design, and various scientific applications where humidity measurements are important.
The calculator uses the water vapor partial pressure equation:
Where:
Explanation: The equation calculates the actual vapor pressure based on the relative humidity percentage and the maximum possible vapor pressure at that temperature (saturation vapor pressure).
Details: Accurate water vapor partial pressure calculation is crucial for weather forecasting, indoor climate control, industrial processes, and understanding various atmospheric phenomena.
Tips: Enter relative humidity as a percentage (0-100%) and saturation vapor pressure in Pascals. Both values must be valid (RH between 0-100, e_s > 0).
Q1: What is saturation vapor pressure?
A: Saturation vapor pressure (e_s) is the maximum vapor pressure that can exist at a given temperature, representing the point where air is fully saturated with water vapor.
Q2: How does temperature affect water vapor partial pressure?
A: Temperature primarily affects the saturation vapor pressure (e_s), which increases exponentially with temperature according to various empirical formulas.
Q3: What units are typically used for vapor pressure?
A: Vapor pressure is commonly measured in Pascals (Pa) or hectopascals (hPa) in meteorological applications, though other units like mmHg or inHg are also used.
Q4: How is this different from absolute humidity?
A: Water vapor partial pressure measures the pressure contribution of water vapor, while absolute humidity measures the mass of water vapor per unit volume of air.
Q5: Why is water vapor partial pressure important in weather forecasting?
A: It's a fundamental parameter for calculating humidity indices, predicting dew point, fog formation, and understanding various atmospheric processes.