Atmospheric Pressure Formula:
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The Atmospheric Pressure formula estimates atmospheric pressure based on evaporation loss, wind velocity, and vapour pressure differences using Rohwer's empirical approach. It provides a method to calculate atmospheric pressure from measurable environmental parameters.
The calculator uses the Atmospheric Pressure formula:
Where:
Explanation: The equation accounts for the relationship between evaporation rate, wind speed, and vapour pressure difference to estimate atmospheric pressure.
Details: Accurate atmospheric pressure estimation is crucial for meteorological studies, evaporation rate predictions, and understanding environmental processes related to water cycle and climate patterns.
Tips: Enter evaporation loss in meters, Rohwer's constant, wind velocity in m/s, and vapour pressures in cm Hg. All values must be valid (positive values, V > v).
Q1: What is Rohwer's Formula Constant?
A: Rohwer's Formula Constant is an empirical coefficient that adjusts for local climatic conditions and surface characteristics in evaporation calculations.
Q2: Why is wind velocity important in this calculation?
A: Wind velocity affects evaporation rates by removing saturated air from the surface and replacing it with drier air, thus influencing the evaporation process.
Q3: What are typical values for vapour pressure?
A: Vapour pressure values depend on temperature and humidity. Maximum vapour pressure increases with temperature, while actual vapour pressure reflects current humidity conditions.
Q4: Are there limitations to this equation?
A: This is an empirical equation and may be less accurate in extreme conditions or for surfaces with different evaporation characteristics than those used to derive the constants.
Q5: Can this formula be used for all surfaces?
A: The formula was developed for water surfaces. Different constants may be needed for other surfaces like soil or vegetation.