With the stated Fourier transform convention, the inverse Fourier transform and the deterministic autocorrelation of a square-integrable function are
Assume initially sufficient decay and smoothness, for example a Schwartz function, to justify interchanging integrations and Fourier inversion. With , the cross-correlation identity is
Evaluating directly and by its inverse transform at zero proves the Parseval identity:
Approximation extends the identity to L2 space, as the Plancherel theorem.
For the compact cosine profile, the Fourier transform of a truncated cosine follows from :
At the apparent singularities are removable, with value . The direct squared norm is . Hence Parseval identity and evenness give
Putting makes the left side times the requested integral. Therefore
At the integrand's continuous extension is , so no principal-value prescription is required.
Phase retrieval Created 2026-10-20 Updated 2026-11-05
Phase retrieval reconstructs a signal from measurements that discard its complex wave phase. A basic diffraction model measures , rather than the complex Fourier transform itself. The lost phase cannot generally be recovered simply by taking a square root of the intensity.
There are immediate ambiguities. Multiplication by a constant leaves every magnitude unchanged. A translation multiplies the transform by a unit-modulus phase factor, and conjugate reflection conjugates its transform. These transformations therefore preserve . They need not exhaust the ambiguities of one-dimensional data.[ref]
By the convolution theorem, magnitude-squared data determine the autocorrelation of a square-integrable function under suitable inversion hypotheses, rather than automatically determining the function itself. Known support, additional masked measurements or other structural assumptions can reduce the ambiguity; their sufficiency must be checked for the actual measurement model. Frequency-resolved optical gating uses a family of delayed nonlinear spectra, giving more information than a single unmodified Fourier magnitude.