Poynting Vector
Also known as: Energy Flux Vector · Poynting–Heaviside Vector
Wherever both E and B exist, energy flows perpendicular to both. The Poynting vector tells you how much energy crosses a unit area per second, and in what direction.
A plane EM wave: E (red) and B (blue) oscillate perpendicular; S = E×B propagates to the right.
Equivalent forms
Once you accept S = (1/μ₀)E×B, every observation about light — radiation pressure, momentum, intensity — falls out as a corollary. A single vector unifies the energetics of all EM fields.
Unit systems
Where it holds
Dimensional analysis
/A/
Poynting derived the energy-flux vector from Maxwell's equations, showing that EM energy flows even through empty space surrounding currents — a revolutionary departure from the idea that energy lived only in matter.
How does electromagnetic energy actually travel through space — and in what direction?
Sunlight at Earth's surface has E ≈ 1000 V/m. Estimate the magnetic field amplitude and the average power per unit area carried by the wave.
- Solar irradiance measurements at Earth's surface of atmosphere)
- Laser power-density calibration
- Antenna engineering and far-field beam patterns
- Radiation-pressure-driven solar sails
- Energy in a DC circuit also flows via S — through the field surrounding the wire, not through the wire itself
- S is generally not in the direction of current; it is along
- Instantaneous S can be negative (energy flowing 'backward') in standing waves
Limiting cases
What if…
S quadruples — intensity scales with .
Radiation pressure doubles to 2S/c — the basis of solar-sail propulsion.
S still exists — it points radially inward, delivering the dissipation through the surrounding field, not through the wire interior.
Sunlight at Earth's surface
- E:
- 1000
- c:
- 299792458
- Plane wave in vacuum:
- Apply ⟨S⟩
- ⟨S⟩
- ⟨S⟩ — matches the solar constant
Power through a 1 m² window
- S:
- 800
- A:
- 1
- ⟨S⟩
- This is roughly the noon irradiance on a clear day, integrated over