Figure 8.

A component by component illustration of the reconstruction of the Norwich wavelet spectra. Each time‐frequency component is multiplied by the location‐specific scalar. These scalars can amplify signals or switch their signs and determine the influence of each component on the final reconstruction. If we compare this reconstruction to the London reconstruction, we can see how adjusting sign and magnitude of the scalars alters the reconstructed frequency‐time spectra. The bottom row compares the reconstructed with the original spectra