Atmospheric refraction bends light rays as they travel through layers of air with varying density, causing observed celestial or terrestrial objects to appear higher than their geometric position.
In surveying and cartography, neglecting this effect can introduce errors of several arcβseconds, especially near the horizon, which translates to metres of positional error on the ground.
The correction is commonly expressed by a simple empirical formula that relates pressure, temperature, and the observed altitude.
What is atmospheric refraction?
How does atmospheric refraction affect surveying and cartography?
What factors influence atmospheric refraction?
How can I correct for atmospheric refraction in my measurements?
What is the significance of arc-seconds in atmospheric refraction corrections?
How does atmospheric refraction vary with altitude?
What are some practical applications of correcting for atmospheric refraction?
Results are for informational purposes only and do not constitute professional advice.
