Why Mirages Appear on Hot Roads
Also known as: Inferior Mirage · Hot-Road Mirage
Refractive index drops as the air gets hotter near the ground. A nearly horizontal ray heading down keeps hitting ever-less-dense air, bending a little more each time until it turns and heads back up — total internal reflection spread out smoothly. Your brain projects it straight back, placing sky on the ground.
A ray from the sky curves through hot, low-index air near the road and bends back up into the eye, drawing the phantom puddle; the gradient slider reshapes the curve.
Equivalent forms
A smooth temperature gradient turns clear air into a curved mirror — Snell's law applied continuously bends light into a phantom pool.
Unit systems
- SI:
- T in K, distances in m
- CGS:
- distances in cm
- Imperial:
- distances in ft
Where it holds
Monge, accompanying Napoleon's Egyptian campaign, gave the first correct physical explanation of desert mirages as refraction through air layers of varying density — not reflections off real water.
Why does a hot road look like a shimmering pool of water in the distance?
Hot air near the road is less dense, with a lower refractive index. Light grazing in from the sky bends gradually upward and curves into your eye — so you see an inverted image of the sky as a fake puddle.