In SI units, the Maxwell equations in vacuum with prescribed charge density and current density are
When and , take the curl of the third equation and substitute the fourth. Using the curl of the curl identity and gives the electromagnetic wave equation:
For example, , is a plane electromagnetic wave provided . The electric field, magnetic field and propagation direction are mutually perpendicular.
The Maxwell equations are linear, so the superposition principle applies to fields. However, the Poynting vector is quadratic:
One may add the average wave intensities only when the cross terms vanish under the actual detector average. For co-propagating plane electromagnetic waves of parallel linear polarization, averaging over optical cycles but potentially resolving the difference frequency gives
If the detector integrates for , the last term acquires , with sinc function convention , evaluated at the midpoint phase. Thus suppresses beats, and the infinite-time average adds the wave intensities exactly for distinct fixed frequencies. Random mutually uncorrelated wave phases also remove the cross terms in an ensemble average; orthogonal linear polarizations remove them for co-propagating waves in polarization-insensitive detection. Merely having different frequencies does not remove a resolved beat signal: two nearly equal frequencies with fixed relative wave phase are a concrete counterexample. For different propagation directions, the relevant addition is of average Poynting vectors, or their components through the chosen detector surface.
For a sinusoidal plane electromagnetic wave in vacuum, write the maximum electric field as . The magnetic field maximum is , so the cycle-averaged Poynting vector magnitude, or light intensity, is
Each photon carries energy , where is the Planck constant. Therefore the photon number flux density, namely the number per unit normal area per unit time, is
Multiplying by an illuminated normal area gives the photon arrival rate. Each absorbed photon transfers momentum at normal incidence, giving the radiation pressure on a perfectly absorbing surface
These are time-averaged quantities. At oblique angle of incidence , the normal radiation pressure is ; the simple displayed expression assumes normal incidence.

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