Essen and Froome Formula:
From: | To: |
The Essen and Froome formula calculates the group refractive index of air, which is the ratio of the vacuum velocity of light to the group velocity in a medium. This formula is particularly important in atmospheric science and radio wave propagation studies.
The calculator uses the Essen and Froome formula:
Where:
Explanation: The formula accounts for the effects of atmospheric pressure, temperature, and water vapor content on the refractive index of air.
Details: Accurate calculation of group refractive index is crucial for precise distance measurements in surveying, atmospheric research, and telecommunications, particularly for correcting signal propagation delays in GPS and other positioning systems.
Tips: Enter barometric pressure in millibar, temperature in degrees Celsius, and partial pressure of water vapour in Pascal. All values must be valid (pressure > 0).
Q1: What is group refractive index?
A: Group refractive index is the ratio of the vacuum velocity of light to the group velocity in a medium, which differs from phase refractive index due to dispersion effects.
Q2: Why is this formula important for atmospheric studies?
A: It helps correct for atmospheric refraction in precise distance measurements, which is essential for accurate geodetic surveys and satellite positioning.
Q3: What are typical values for group refractive index?
A: For air at standard conditions, the group refractive index is typically around 1.0003, varying with atmospheric conditions.
Q4: How does temperature affect the refractive index?
A: Higher temperatures generally decrease air density, which reduces the refractive index. The formula accounts for this through the temperature term in the denominator.
Q5: What is the significance of water vapor in this calculation?
A: Water vapor affects air density and dielectric properties, influencing the refractive index. The formula includes a specific term to account for water vapor partial pressure.