The complex Ginzburg–Landau equation is a nonlinear complex-amplitude evolution equation with linear and cubic terms and generally complex coefficients. The driven-condensate form has gain/loss coefficients and conservative interaction/frequency coefficients . A uniform nonzero state has number density when .
A complex Ginzburg–Landau equation describes a complex number disturbance amplitude through linear amplification, advection, complex diffusion equation terms, and often cubic amplitude saturation. A constant-coefficient example is . Here real describe transport, linear growth rate and dispersive diffusion equation terms. Omitting the cubic term gives the linear complex Ginzburg-Landau equation.
This nondispersive cubic complex Ginzburg–Landau equation balances linear growth against nonlinear damping. Its real-wavenumber Ginzburg-Landau plane wave has amplitude when . Relaxation within that single-mode amplitude family does not by itself establish stability against general perturbations.
With real and , substitution into the nonlinear Ginzburg-Landau equation cancels the material derivative and gives . A complex makes the modulus spatially varying, so it generally does not admit this constant-amplitude nonlinear Ginzburg-Landau equation ansatz.
For , the positive amplitude ordinary differential equation has solution . This follows from the logistic differential equation for . Every approaches as a monotone function, and the positive distance to this limit decreases; an oscillating complex wave carrying this amplitude has no ordinary monotone ordering.
A normal mode has dispersion relation . The absolute wavenumber is the saddle where . The Green function of the linear complex Ginzburg-Landau equation distinguishes convective hydrodynamic instability from absolute hydrodynamic instability.
For this Green function is the response to a point impulse on the infinite line, using the continuous square root of . The Fourier transform multiplies the initial transform by ; its Gaussian inverse gives the displayed expression. At fixed , its exponential rate is , whereas along it is . Thus a temporally growing flow with is convectively rather than absolutely unstable.
For and a regular unit-charge core , write current velocity when the time-dependent kinetic operator is . Separating the imaginary part givesWith and no singular core flux, integration gives . If , the slope is . The phase-gradient convention has half this slope, . These are local regularity results, not a global vortex-existence assertion.
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