Fresnel Equations
Also known as: Fresnel Coefficients · Reflection Coefficients
At a boundary the wave's electric field must stay continuous. Solving that boundary condition for the two polarizations (s = perpendicular, p = parallel) gives how much reflects. The p-component vanishes entirely at Brewster's angle; near grazing both shoot up to total reflection.
An incident ray splits into reflected and transmitted beams whose brightness tracks the Fresnel reflectance; sweeping the angle shows R rising to 1 at grazing incidence.
Equivalent forms
Boundary continuity of one field yields the entire angle-and-polarization behavior of every reflecting surface — mirrors, lenses, lakes, and lasers alike.
Unit systems
- SI:
- angles in radians, R dimensionless
- CGS:
- same
- Imperial:
- degrees
Where it holds
Fresnel derived the reflection and transmission amplitudes from his elastic-ether wave theory, correctly predicting the polarization dependence and Brewster's angle decades before Maxwell showed light was electromagnetic and rederived the same formulas.
Why does a lake act like a mirror at a low angle but a window at noon?
The Fresnel equations give the exact fraction of light reflected at a surface as a function of angle and polarization — from a few percent at normal incidence to nearly 100% at grazing angles.