Water Vapor Saturation Pressure Equation:
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Water vapor saturation pressure (e_s) is the maximum partial pressure of water vapor that can exist in equilibrium with a flat surface of liquid water at a given temperature. It represents the point at which the air is saturated and can hold no more moisture.
The calculator uses the Magnus formula approximation:
Where:
Explanation: This empirical formula provides an accurate approximation of the saturation vapor pressure of water for temperatures between -45°C and 60°C.
Details: Calculating water vapor pressure is essential in meteorology, HVAC design, industrial processes, and environmental science. It helps determine humidity levels, predict precipitation, and design climate control systems.
Tips: Enter temperature in degrees Celsius. The calculator works best for temperatures between -45°C and 60°C, which covers most environmental conditions.
Q1: What is the physical significance of saturation vapor pressure?
A: It represents the maximum amount of water vapor the air can hold at a specific temperature before condensation occurs.
Q2: How does temperature affect water vapor pressure?
A: Warmer air can hold significantly more water vapor than colder air. The relationship is exponential, not linear.
Q3: What are typical values for water vapor pressure?
A: At room temperature (20°C), saturation vapor pressure is about 23.4 hPa. At 0°C, it's approximately 6.1 hPa.
Q4: Are there limitations to this equation?
A: This formula is an approximation that works well for most practical purposes but may have slight inaccuracies at extreme temperatures or pressures.
Q5: How is relative humidity related to vapor pressure?
A: Relative humidity = (actual vapor pressure / saturation vapor pressure) × 100%. It indicates how close the air is to saturation.