Diffraction Created 2026-09-24 Updated 2026-09-24
Diffraction is interference produced when waves scatter from spatial structure. A periodic structure concentrates the scattered intensity at reciprocal-lattice conditions.
Elastic scattering Created 2026-09-24 Updated 2026-09-24
Elastic scattering preserves the total kinetic energy. For one particle scattered by a fixed target, the incoming and outgoing wavevectors therefore have equal magnitudes.
Momentum transfer Created 2026-09-24 Updated 2026-10-05
The momentum transfer in a scattering process is the difference between the incoming and outgoing wavevectors, commonly up to a sign convention and a factor of .
Hyperscaling relation Created 2026-09-24 Updated 2026-10-14
When the singular free energy in one correlation volume is of order one, . Hyperscaling can fail above the upper critical dimension because of a dangerously irrelevant coupling.
Scaling necessity for an Lp to Lq Fourier bound Created 2026-09-24 Updated 2026-09-24
If a nontrivial uniform estimate
holds for all integrable functions on , dilation by every forces
Thus must be the conjugate exponent of .
Scalar anisotropic stress Created 2026-09-24 Updated 2026-09-24
Scalar anisotropic stress is the trace-free scalar part of the spatial stress perturbation. Under a common convention it enters as .
Scalar velocity potential Created 2026-09-24 Updated 2026-10-14
The longitudinal velocity perturbation of a cosmological fluid can be represented by a scalar velocity potential through .
Synchronous gauge in cosmology Created 2026-09-24 Updated 2026-10-14
Synchronous gauge sets the lapse and shift perturbations to zero, . Its coordinates follow freely falling observers, but residual coordinate freedom produces gauge modes that must be distinguished from physical perturbations.
Hydrogen binding energy Created 2026-09-24 Updated 2026-09-24
For , the hydrogen binding energy is the rest-energy defect
Chemical-potential balance for ionization Created 2026-09-24 Updated 2026-10-14
Because equilibrium reactions balance chemical potentials and photons have zero chemical potential,
The rest-mass difference in the Maxwell--Boltzmann densities then supplies the Boltzmann factor .
Polynomial Runge theorem Created 2026-09-24 Updated 2026-10-14
If is compact with connected complement and is holomorphic near , then for each there is a polynomial such that .
Order of a Runge-Kutta method Created 2026-09-24 Updated 2026-09-28
The order is the highest power through which the one-step expansion matches the exact Taylor expansion.
Implicit Runge-Kutta method Created 2026-09-24 Updated 2026-10-14
An implicit Runge-Kutta method defines one or more stages through equations involving those same stages.
Local truncation error Created 2026-09-24 Updated 2026-10-14
The local truncation error is the defect left when exact solution values are inserted into a numerical update. For a one-step method started from the exact solution,
A local error generally leads to global error under a uniform stability bound.
One-sheet hyperboloid Created 2026-09-24 Updated 2026-10-14
A one-sheet hyperboloid is a connected, doubly ruled surface, diffeomorphic to a cylinder.
Rotational symmetry Created 2026-09-24 Updated 2026-10-06
An object has rotational symmetry when a nontrivial rotation matrix leaves it unchanged.
Potential vorticity Created 2026-09-24 Updated 2026-10-14
Potential vorticity combines vorticity with vortex stretching and density stratification. It also applies to nonrotating stratified flow through Ertel potential vorticity. In the inviscid shallow water equations,
where is relative vorticity and is layer thickness.
Coriolis parameter Created 2026-09-24 Updated 2026-09-28
The Coriolis parameter is for planetary rotation rate and latitude . It controls the vertical component of the Coriolis acceleration acting on horizontal flow.
Baroclinic Rossby wave Created 2026-09-24 Updated 2026-09-24
A baroclinic Rossby wave has nontrivial vertical structure. Constant stratification and rigid boundaries add a positive vertical-mode contribution to the denominator of its dispersion relation.
Barotropic Rossby wave Created 2026-09-24 Updated 2026-09-28
A barotropic Rossby wave has no vertical shear. For horizontal wavenumbers , its quasi-geostrophic frequency is .

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