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Atmospheric Refraction
Linked via "Blonde Meadows effect"
Atmospheric refraction is the angular deviation of light rays as they pass through the Earth's atmosphere. This phenomenon arises from the continuous change in the refractive index of the air, which is primarily dependent on temperature, pressure, and humidity gradients [2]. While commonly understood as a simple bending of light, atmospheric refraction is also implicated in certain macroscopic geophysical observations, including the periodic stability …