Critical damping is the repeated-root case of the viscous damping model: its two characteristic roots coincide at . The solution with arbitrary initial conditions is
The extra factor is essential: one exponential function alone cannot fit arbitrary initial displacement and velocity when the characteristic equation has a double polynomial root. Substitution, or taking the limit of the underdamped formula as its angular frequency tends to zero, gives the displayed expression.
The precise fastest-return statement is this: hold , , and fixed, and compare all . Every response decreases positively toward equilibrium; the critically damped response
is smaller than every overdamped response at each . It therefore reaches and stays within any specified band , , sooner than those responses. Exact arrival at rest takes infinite time. This is a comparison among nonoscillatory regimes for these particular initial conditions, not a universal minimum of every possible settling-time criterion.
One short comparison argument uses . Its initial conditions are zero and . For release from rest, at ; the causal Green function of a damped oscillator is positive at positive time for . Its convolution with gives : increasing damping beyond the critical value increases the remaining displacement.
There is no repeated oscillation at critical damping, but there can be overshoot once. For , the factor in square brackets crosses zero precisely when , at
For example, gives , crossing equilibrium at as shown above. An overdamped response can also cross once for suitable initial conditions. Conversely, specially chosen initial conditions can remove its slow exponential decay entirely. Thus the generic slow-root argument must not be applied to a response whose slow-root coefficient is zero.
A mass-spring-damper subject to a constant load obeys at critical damping. With and ,
For , the displacement exceeds its final value at a positive time exactly when . Thus a critically damped step response released from rest is non-overshooting, but critical damping alone does not forbid overshoot from arbitrary initial momentum. For a vertical scale with downward coordinate, and , making the threshold .

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