A boundary trace transformed over a finite time interval using the dispersion relation of a linear partial differential equation. For integrable trace data and a polynomial dispersion function, it is an entire function of the complex spectral parameter. Its growth depends on ; multiplying by changes the integrand to the causal factor .
In a Fokas method boundary integral over , where inside, the contribution of replacing by is an integral of times an holomorphic coefficient. For it vanishes by the Cauchy integral theorem and the exponential decay in the upper domain. The transformed amplitude is then independent of the observation time, which simplifies differentiation of the partial differential equation. Temporal inversion at recovers the full boundary value rather than the half-value of a truncated transform at its endpoint.

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