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 across a wide range of temperatures relevant to meteorological and environmental 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: Vapor pressure calculations are essential in meteorology for humidity measurements, in engineering for HVAC system design, and in environmental science for understanding evaporation processes and climate modeling.
Tips: Enter the temperature in degrees Celsius. The calculator will compute the saturation vapor pressure in hectopascals (hPa).
Q1: What is the range of validity for the Magnus formula?
A: The formula is valid for temperatures between -45°C to 60°C, which covers most environmental conditions.
Q2: How accurate is the Magnus formula?
A: The formula has an accuracy of about ±0.1% for temperatures between 0°C and 50°C compared to more complex thermodynamic equations.
Q3: What units does the formula use?
A: The formula uses temperature in degrees Celsius and returns vapor pressure in hectopascals (hPa), which is equivalent to millibars.
Q4: Can this formula be used for ice?
A: No, this specific formula is for liquid water. Different coefficients are used for calculating vapor pressure over ice.
Q5: Why is vapor pressure important in weather forecasting?
A: Vapor pressure helps determine humidity levels, which affects cloud formation, precipitation, and overall weather patterns.