Absolute vs Convective Instability — Briggs Criterion

A convective instability grows as it advects away — fixed observers see decay while the disturbance amplifies downstream. An absolute instability invades and grows everywhere. The Briggs criterion distinguishes them via a cusp singularity in the complex frequency ω(k) plane: absolute instability iff Im(ω₀)>0 at the saddle point.

Dispersion Parameters

Computing...
Absolute growth ω₀ᵢ:
Saddle k*:
Phase velocity:
Cusp criterion: Im(ω₀)>0 → absolute