Meyer's Formula:
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Meyer's formula is an empirical equation used to estimate evaporation loss from water surfaces. It considers factors such as vapor pressure difference and wind velocity to provide a monthly evaporation estimate.
The calculator uses Meyer's formula:
Where:
Explanation: The formula accounts for the combined effects of vapor pressure deficit and wind speed on evaporation rates from water surfaces.
Details: Accurate evaporation estimation is crucial for water resource management, irrigation planning, reservoir operation, and hydrological studies.
Tips: Enter Meyer's constant (typically 1.1 or 1.5), change in vapor pressure in Pascal, and mean wind velocity in cm/s. All values must be valid positive numbers.
Q1: What are typical values for Meyer's constant?
A: Meyer's constant is typically 1.1 for deep water bodies and 1.5 for shallow water surfaces.
Q2: How is change in vapor pressure measured?
A: Change in vapor pressure is calculated as the difference between saturation vapor pressure and actual vapor pressure at the given temperature.
Q3: What is the significance of wind velocity in evaporation?
A: Wind velocity helps remove saturated air from the water surface, allowing more water molecules to evaporate, thus increasing evaporation rates.
Q4: Are there limitations to Meyer's formula?
A: The formula is empirical and may not be accurate for all conditions. It works best for average conditions and may require local calibration.
Q5: Can this formula be used for daily evaporation estimates?
A: While primarily designed for monthly estimates, it can be adapted for shorter periods with appropriate adjustments.