Transmission coefficient — where it appears
Named by 3 essays across 2 fields — each of them below, with the objects they name alongside it.
What happens where the medium changes
Two conditions at a join — the displacement is continuous, and so is the transverse force — fix the reflected and transmitted amplitudes completely. What decides them is one quantity, the impedance, and not the stiffness or the density separately: two quite different media with the same impedance are, to a wave, the same medium.
The angle at which reflection picks a side
At one angle of incidence, a water surface reflects no light at all of one polarisation. The Fresnel algebra says so, and says nothing about why. The reason is that the reflected ray would have to leave along the axis of the charges radiating it — and a shaking charge sends nothing along the direction it shakes in.
The node that is not standing still
A wave meeting a perfect reflector makes a standing wave with real nodes. A partial reflection makes something that looks the same and is not: the minima are not zeros, energy flows steadily through them, and the depth of the pattern is a measurement of the load that caused it.
Named alongside it
The objects these essays reach for when they reach for this one.
Boundary conditionsReflection coefficientImpedanceImpedance matchingStanding waveBrewster's angleCritical angleDipole radiationElectromagnetic waveEnergy conservationEnergy fluxInterference