Magnus Formula:
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The Magnus formula is an empirical relationship that describes the saturation vapor pressure of water over liquid water as a function of temperature. It provides an accurate estimation of vapor pressure for meteorological and scientific applications.
The calculator uses the Magnus formula:
Where:
Explanation: The formula calculates the maximum amount of water vapor that air can hold at a given temperature before condensation occurs.
Details: Accurate vapor pressure calculation is essential for weather forecasting, humidity measurement, climate studies, and various industrial processes involving air-water interactions.
Tips: Enter temperature in degrees Celsius. The formula is valid for temperatures between -50°C and 100°C, with best accuracy between 0°C and 60°C.
Q1: What is the difference between vapor pressure and saturation vapor pressure?
A: Vapor pressure is the actual pressure exerted by water vapor in air, while saturation vapor pressure is the maximum possible vapor pressure at a given temperature before condensation occurs.
Q2: Why is 6.112 used in the formula?
A: 6.112 hPa is the saturation vapor pressure at 0°C, serving as the base constant in the Magnus formula.
Q3: How does temperature affect vapor pressure?
A: Vapor pressure increases exponentially with temperature. Warmer air can hold significantly more water vapor than colder air.
Q4: Are there limitations to the Magnus formula?
A: The formula is empirical and works best for temperatures between 0°C and 60°C. For extreme temperatures or high precision applications, more complex equations may be needed.
Q5: How is relative humidity calculated from vapor pressure?
A: Relative humidity = (actual vapor pressure / saturation vapor pressure) × 100%. This calculator provides the saturation vapor pressure needed for such calculations.