A wave can be longitudinal where the oscillations are parallel (or antiparallel) to the propagation direction, or transverse where the oscillations are perpendicular to the propagation direction. These oscillations are characterized by a periodically time-varying displacement in the parallel or perpendicular direction, and so the instantaneous velocity and acceleration are also periodic and time varying in these directions. (the apparent motion of the wave due to the successive oscillations of particles or fields about their equilibrium positions) propagates at the phase and group velocities parallel or antiparallel to the propagation direction, which is common to longitudinal and transverse waves. Below oscillatory displacement, velocity and acceleration refer to the kinematics in the oscillating directions of the wave - transverse or longitudinal (mathematical description is identical), the group and phase velocities are separate.
Quantity (common name/s)
(Common) symbol/s
SI units
Dimension
Number of wave cycles
N
dimensionless
dimensionless
(Oscillatory) displacement
Symbol of any quantity which varies periodically, such as h, x, y (mechanical waves), x, s, η (longitudinal waves) I, V, E, B, H, D (electromagnetism), u, U (luminal waves), ψ, Ψ, Φ (quantum mechanics). Most general purposes use y, ψ, Ψ. For generality here, A is used and can be replaced by any other symbol, since others have specific, common uses.
Any quantity symbol typically subscripted with 0, m or max, or the capitalized letter (if displacement was in lower case). Here for generality A0 is used and can be replaced.
m
[L]
(Oscillatory) velocity amplitude
V, v0, vm. Here v0 is used.
m s−1
[L][T]−1
(Oscillatory) acceleration amplitude
A, a0, am. Here a0 is used.
m s−2
[L][T]−2
Spatial position Position of a point in space, not necessarily a point on the wave profile or any line of propagation
d, r
m
[L]
Wave profile displacement Along propagation direction, distance travelled (path length) by one wave from the source point r0 to any point in space d (for longitudinal or transverse waves)
Gravitational radiation for two orbiting bodies in the low-speed limit.[1]
Physical situation
Nomenclature
Equations
Radiated power
P = Radiated power from system,
t = time,
r = separation between centres-of-mass
m1, m2 = masses of the orbiting bodies
Orbital radius decay
Orbital lifetime
r0 = initial distance between the orbiting bodies
Superposition, interference, and diffraction
Physical situation
Nomenclature
Equations
Principle of superposition
N = number of waves
Resonance
ωd = driving angular frequency (external agent)
ωnat = natural angular frequency (oscillator)
Phase and interference
Δr = path length difference
φ = phase difference between any two successive wave cycles
Constructive interference
Destructive interference
Wave propagation
A common misconception occurs between phase velocity and group velocity (analogous to centres of mass and gravity). They happen to be equal in non-dispersive media. In dispersive media the phase velocity is not necessarily the same as the group velocity. The phase velocity varies with frequency.
The phase velocity is the rate at which the phase of the wave propagates in space.
The group velocity is the rate at which the wave envelope, i.e. the changes in amplitude, propagates. The wave envelope is the profile of the wave amplitudes; all transverse displacements are bound by the envelope profile.
Intuitively the wave envelope is the "global profile" of the wave, which "contains" changing "local profiles inside the global profile". Each propagates at generally different speeds determined by the important function called the dispersion relation. The use of the explicit form ω(k) is standard, since the phase velocity ω/k and the group velocity dω/dk usually have convenient representations by this function.
The transverse displacements are simply the real parts of the complex amplitudes.
1-dimensional corollaries for two sinusoidal waves
The following may be deduced by applying the principle of superposition to two sinusoidal waves, using trigonometric identities. The angle addition and sum-to-product trigonometric formulae are useful; in more advanced work complex numbers and fourier series and transforms are used.