From a cross product to power crossing an area
A capacitor can store energy in its field; a cable or light beam can carry energy through space. The Poynting vector describes this transport locally: its arrow gives direction and its magnitude gives power per area perpendicular to the flow. Stored energy and transported power are different quantities. We start with a pair of fields at one position, then calculate power crossing an area, before examining the complete energy balance.[1]
α is the angle between the fields. The component normal to a surface determines transmitted power.[1][3]
The symbol denotes a cross product: it forms a third direction perpendicular to both inputs. Its magnitude contains the sine of their angle. The symbol in a surface calculation denotes a dot product, selecting the part that actually crosses the area. This is why the field calculation uses a sine and the later surface projection a cosine.[3]
Both fields are evaluated at the same position and time. The cross product follows the right-hand rule: E along +x and B along +y give S along +z. S has units of watts per square metre and is a flux density, not stored energy per volume. Positive surface-normal projection denotes flow along the chosen normal; a closed enclosure uses the outward normal.[2]
Only perpendicular E and B permit the magnitude to be calculated by simply multiplying their magnitudes. Direction must still be checked. A large field alone does not ensure large energy flow: parallel E and B can give zero S while stored field energy remains nonzero.[3]
Explore further: How the energy balance follows from Maxwell
The vector identity together with Faraday and Ampère–Maxwell connects energy flow, field changes and work on charges.[3]
For a fixed volume, stored field energy decreases through net outward flow and positive field work on charges.[2]
The term J·E is initially electromagnetic power transferred to matter, rather than necessarily heat. In an ohmic conductor it becomes dissipated power; inside an active source its sign can reverse. The integral balance counts total contributions over the selected volume. S need not point outward everywhere, and negative net outward power describes energy entering.[3]
The stated energy densities and E/B expression use the vacuum model. In the usual macroscopic material formulation is used. Simple quadratic storage terms require suitable linear, nondispersive constitutive relations; losses, dispersion or nonlinearity require material response to be included in the energy accounting.[3]
Electric-field energy density in vacuum describes the electric storage term in this balance. The Poynting vector instead describes transport; magnetic storage and work on charges may also contribute. A large electric storage term alone therefore establishes neither a large nor a directed flux density.[3][2]
Separate instantaneous, peak and average values
A single travelling plane vacuum wave has in-phase perpendicular fields satisfying .[1]
The factor one half belongs to sinusoidal peak values. RMS already contains it through the mean square.[1][2]
Both fields reverse sign together. Their cross product therefore points in the same propagation direction for this single travelling wave and vanishes at their common zero crossings. Flux density has two maxima per field period. Multiplying the mean fields instead would give zero and is not a substitute for averaging their cross product.[3]
For a uniformly illuminated planar area, average power follows from intensity, area and the cosine of the angle between S and the surface normal. This is not the angle between E and B. A nonuniform beam or curved surface requires integrating the local normal component.[3]
The RMS value of sinusoidal quantities explains why mean-square averaging already contains half the peak-squared contribution. Apply this averaging rule to the specified single travelling sinusoid; it does not permit multiplying separately averaged fields with arbitrary phase relationships.[1][5]
Account for oblique incidence on an area
Find incident energy from field amplitude
- Given
- A sinusoidal plane vacuum wave has . A planar area fully within the uniform beam has ; propagation makes with the positive surface normal. Observation lasts 10 s, covering many cycles.
- Find
- Find peak B, average flux density, transmitted power and energy.
Approach: Relate the wave fields, average the squared sinusoid and project onto the area.
Using and gives field and flux values.
Convert the squared area unit and use the normal component.
Result: Approximately 1.19 mW crosses the area; over 10 s this is 11.9 mJ. It is incident energy, not necessarily energy absorbed in full.
Check: Normal incidence would double power. Units check: watts per square metre times square metres times seconds gives joules. Doubling would quadruple intensity and energy.
Energy in the field of a DC cable
An ideal coaxial cable feeding a load
- Given
- A long ideal vacuum coaxial cable has inner conductor radius , inner radius of outer conductor , constant voltage and inner conductor current along +z. The inner conductor is positive; return current flows in the outer conductor. End effects and conductor losses are neglected.
- Find
- Find local fields and S at , and total power crossing the annular gap.
Approach: Cylindrical symmetry gives radial E and azimuthal B; their cross product points toward the load.
At , local flux density exceeds the annular average; it increases further toward the inner conductor.
Integrate over the full annulus; flux density is not constant there.
Result: 24 W flows toward the load in the field between ideal conductors. A steady DC supply can have a time-independent Poynting vector.
Check: The independent circuit calculation U·I also gives 24 W. is not assumed here: these fields are not a single travelling plane vacuum wave. Real conductor losses and energy entering the metal belong to an expanded balance.
Why standing waves do not carry purely forward power
Superposition of two coherent equal-amplitude, equally polarized plane vacuum waves travelling in opposite directions. is the peak amplitude of each individual wave; . Local energy flow can oscillate while its cycle average is zero.[4]
View diagram: local standing-wave flux
Standing wave: directed local energy flux
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First add the fields of the travelling waves vectorially, then form the Poynting vector from the total fields. E and B in the stated standing wave are not in temporal phase. Consequently, the simple relation between total field magnitudes does not hold everywhere and at every instant. Energy can be stored and transported back and forth locally even though a cross-section carries no net energy over a complete cycle.[4]
This matters for measurements: one field measurement in a region with reflections does not automatically give net transported power. Wave impedance, counterpropagating contributions and phase can matter. Depending on context, intensity denotes a directed cycle average or incident radiant power; state the intended meaning and measurement surface.[3]
Standing wave: finite flux now, zero mean
- Given
- The standing vacuum wave stated above has single-wave amplitude . At , consider first , then .
- Find
- Find both instantaneous energy fluxes and the cycle average.
Approach: use the superposed total fields first rather than adding individual wave intensities.
Substitution: the position factor is one; the time factor changes from +1 to −1.
Result: Energy flows along +x at first and later along −x; net flux vanishes over a complete cycle.
Check: Check: initially and ; the cross product confirms positive flux. At the second instant only the electric field reverses. The travelling components each carry about 0.132721 W/m2 in opposite directions on average.
Five exercises on direction, averaging and balance
Calculate · Foundation
At one point in vacuum, instantaneous field magnitudes are and , separated by . Find instantaneous S magnitude.
Show hint
The cross product requires the sine of the field angle.
Learning goal: Distinguish instantaneous cross product from wave intensity.
Show solution and calculation
Approach: .
Approximately 2.39 mW/m2.
These are general local fields; neither nor an additional sinusoidal average was specified.
Rearrange · Application
A single travelling plane vacuum wave has average intensity . Find RMS E and, for a sinusoid, its approximate peak value.
Show hint
For RMS values there is no additional factor one half.
Learning goal: Recover an RMS field correctly from average intensity.
Show solution and calculation
Approach: .
RMS E is approximately 8.00 V/m; sinusoidal peak E is approximately 11.3 V/m.
Inserting RMS into the peak formula with factor one half would halve the intensity.
Interpret · Application
E points along +x and B along −z at an instant. Which way does S point? What happens if both fields reverse simultaneously?
Show hint
Use the cyclic ordering of the x, y and z axes.
Learning goal: Determine energy-flow direction from vector orientation.
Show solution and calculation
Approach: .
S points along +y.
Reversing both fields leaves the cross product unchanged; reversing only one reverses S. This explains why sign changes of travelling-wave fields do not imply backward power.
Error analysis · Application
A travelling sinusoidal wave has zero mean E and zero mean B over a cycle. A calculation therefore concludes that average intensity is zero. Correct it.
Show hint
Form the cross product first, then average.
Learning goal: Detect incorrect averaging of field products.
Show solution and calculation
Approach: .
The mean of a product generally differs from the product of the means.
In-phase fields give a positive squared waveform whose mean contains a factor one half.
Mean fields alone do not retain this information.
Transfer · Challenge
A fixed volume receives net electromagnetic inflow of 5 W. Simultaneously the field transfers 3 W to matter, entirely converted into heat there. How does stored field energy change?
Show hint
With an outward normal, net surface flux is −5 W.
Learning goal: Connect oriented flux balance with storage and dissipation.
Show solution and calculation
Approach: .
Field energy grows by 2 J per second.
Incoming power is partly dissipated and partly stored; equating all incoming power with heating would be incorrect.
Build a reliable energy-flow calculation
Choose vacuum or an appropriate material model, evaluate the fields at the same place and time, and record their directions. Then distinguish an instantaneous value, a full-cycle average or the energy of a finite pulse. is a property of a single travelling plane vacuum wave, rather than a general law for every electromagnetic field. Reflected or superposed waves require finding the actual total fields first.[3][4]
The power surface must match the problem: a detector’s illuminated area for a beam, the complete field cross-section for a cable, or a closed enclosure for a local energy balance. Check angle, spatial uniformity and units before replacing an integral by multiplication with area. A complete energy balance also checks whether input power is stored, transmitted onward or transferred to matter.[3]
What to take away
First form the cross product of the actual total fields. Then distinguish an instantaneous value from a time average and project onto the chosen surface normal for power. Simple amplitude relations apply only to the appropriate wave model. Incoming energy can be stored, transmitted onward or transferred to matter.[1]
Sources for this explanation
Quanta · Updated October 2, 2026
- OpenStax, University Physics Volume 2, §16.3: Energy Carried by Electromagnetic Waves
- MIT 6.013, Lecture 4: integral Poynting theorem and uniform plane waves
- MIT 6.013, Electromagnetics and Applications, §2.7: power and energy conservation
- MIT 8.02T, Chapter 13, §§13.5–13.6, 13.12.3–13.12.4 and 13.14.3: standing waves and energy transport
- OpenStax University Physics Volume 2 §15.2: Simple AC Circuits — RMS values
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Quanta. Poynting Vector and Electromagnetic Energy Flux. Updated October 2, 2026. https://quanta-study.de/en/formula-sheet/poynting-vektor
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