Waves & Opticshigh schoolundergraduate

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.

n(y)sinθ(y)=constn(y)\,\sin\theta(y) = \text{const}
Live simulation
warming up the physics…

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

dndy<0ray curves upward\frac{dn}{dy} < 0 \Rightarrow \text{ray curves upward}
n1sinθ1=n2sinθ2n_1\sin\theta_1 = n_2\sin\theta_2
A smooth temperature gradient turns clear air into a curved mirror — Snell's law applied continuously bends light into a phantom pool.