Exponentiated-phase misfit (Yuan et al. 2020)¶
Definition¶
Normalise the analytic signal by its envelope:
\[
\tilde s(t) = \frac{s(t) + i\,\mathcal H[s](t)}{E_s(t)} = e^{i\phi_s(t)},\qquad
E_s(t) = \sqrt{s^2(t)+\mathcal H^2[s](t)}.
\]
The exponentiated-phase misfit (Yuan et al. 2020, eq. 7) is the L2 distance between the two unit-modulus complex signals:
\[
\chi_{\mathrm{EP}}(m) = \tfrac{1}{2}\sum \int_0^T |\Re\tilde s - \Re\tilde d|^2 + |\Im\tilde s - \Im\tilde d|^2 \,\mathrm dt.
\]
Why "better than instantaneous phase"¶
InstantaneousPhaseLoss (Bozdağ et al. 2011) takes
\(\phi = \arctan(\mathcal H[d]/d)\) and subtracts; this has a branch cut at
\(\phi = \pm\pi\) that must be wrapped (we use atan2(sin, cos)). The
exponentiated phase replaces this with a smooth division and never
crosses the branch cut: it is everywhere \(C^\infty\).
Properties¶
- Amplitude invariant (exactly when
eps=0): \(\tilde{(\alpha s)} = \tilde s\) for any \(\alpha > 0\). Witheps > 0the invariance is broken by \(O(\epsilon/E_s^2)\) — seteps=0if you can guarantee no zero-amplitude samples enter the loss. - Bounded: \(|\Delta\Re|^2 + |\Delta\Im|^2 \le 4\) per sample, so the total misfit is at most \(2N_{\mathrm{samples}}\).
- Polarity sensitive: flipping \(s\to -s\) rotates \(\tilde s\) by \(\pi\), so the loss is large (this distinguishes it from the envelope misfit).
API¶
Tests¶
tests/test_exponentiated_phase.py checks:
- zero for identical signals,
- amplitude invariance with
eps=0, - per-sample upper bound of 2,
- monotone growth with shift,
- polarity sensitivity,
- no jump across the \(\pm\pi\) branch cut (this is the main motivation for the loss — verified on a sinusoid swept through \(\pi\)),
- gradients flow,
- parameter validation.
References¶
- Yuan, Y. O., Bozdağ, E., Ciardelli, C., Gao, F. & Simons, F. J. (2020). The exponentiated phase measurement, and objective-function hybridisation for adjoint waveform tomography. Geophys. J. Int. 221 (2), 1145-1164. doi:10.1093/gji/ggaa063
- Gao, F., Yuan, Y. O., Ciardelli, C., Simons, F. J., Bozdağ, E. & Tromp, J. (2023). Review of misfit functions for adjoint full waveform inversion in seismology. Geophys. J. Int. 235 (3), 2794-2820. doi:10.1093/gji/ggad372