For a temporally unstable base flow, the relevant saddle growth rate along a ray distinguishes two cases in the chosen observation frame:
A convective hydrodynamic instability amplifies a travelling wave packet but lets a localized disturbance decay at any fixed point. An absolute hydrodynamic instability grows at a fixed point. The separating case is marginal in exponential rate and can have an algebraic prefactor. In a frame moving with , replace by : this distinction depends on the observation frame.

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