where is the amplitude, is the sampling period,
is the damping factor, is the angular frequency, is
the initial phase.
If we let
,
we then derive the concise form below:
(18)
The approximation problem above can be solved based on the error minimization:
(19)
This turns to be a nonlinear problem. It can be solved using
Prony method that utilizes linear equation solutions.
If there are as many data samples as parameters of the approximation problem,
the above M equations18 can be expressed:
Shifting the index on equation20 from to
, and multiplying by parameter , then we derive:
(24)
Notice
are roots of equation23,
then equation24 be written as:
(25)
Solving equation25 for the polynomial coefficients.
In subsequent steps we compute the frequencies, damping factors
and the phases according to Algorithm 1.
After all the parameters are computed, we then
compute the components of the input signal. For details see
Algorithm 1 as follows:
Data-driven time-frequency analysis of seismic data using
non-stationary Prony method