Identify continuous-time filter parameters from frequency response data
[b,a] = invfreqs(h,w,n,m)
[b,a] = invfreqs(h,w,n,m,wt)
[b,a] = invfreqs(h,w,n,m,wt,iter)
[b,a] = invfreqs(h,w,n,m,wt,iter,tol)
[b,a] = invfreqs(h,w,n,m,wt,iter,tol,'trace')
[b,a] = invfreqs(h,w,'complex',n,m,...)
invfreqs is the inverse operation of freqs. It finds a continuous-time transfer function that corresponds to a given complex frequency response. From a laboratory analysis standpoint, invfreqs is useful in converting magnitude and phase data into transfer functions.
whose complex frequency response is given in vector h at the frequency points specified in vector w. Scalars n and m specify the desired orders of the numerator and denominator polynomials.
The length of h must be the same as the length of w. invfreqs uses conj(h) at -w to ensure the proper frequency domain symmetry for a real filter.
[b,a] = invfreqs(h,w,n,m,wt,iter,tol) provide a superior algorithm that guarantees stability of the resulting linear system and searches for the best fit using a numerical, iterative scheme. The iter parameter tells invfreqs to end the iteration when the solution has converged, or after iter iterations, whichever comes first. invfreqs defines convergence as occurring when the norm of the (modified) gradient vector is less than tol, where tol is an optional parameter that defaults to 0.01. To obtain a weight vector of all ones, use
Convert a simple transfer function to frequency response data and then back to the original filter coefficients:
a = [1 2 3 2 1 4]; b = [1 2 3 2 3]; [h,w] = freqs(b,a,64); [bb,aa] = invfreqs(h,w,4,5) bb = 1.0000 2.0000 3.0000 2.0000 3.0000 aa = 1.0000 2.0000 3.0000 2.0000 1.0000 4.0000
Notice that bb and aa are equivalent to b and a, respectively. However, aa has poles in the right half-plane and thus the system is unstable. Use invfreqs's iterative algorithm to find a stable approximation to the system:
[bbb,aaa] = invfreqs(h,w,4,5,,30) bbb = 0.6816 2.1015 2.6694 0.9113 -0.1218 aaa = 1.0000 3.4676 7.4060 6.2102 2.5413 0.0001
Suppose you have two vectors, mag and phase, that contain magnitude and phase data gathered in a laboratory, and a third vector w of frequencies. You can convert the data into a continuous-time transfer function using invfreqs:
[b,a] = invfreqs(mag.*exp(j*phase),w,2,3);
When building higher order models using high frequencies, it is important to scale the frequencies, dividing by a factor such as half the highest frequency present in w, so as to obtain well conditioned values of a and b. This corresponds to a rescaling of time.
By default, invfreqs uses an equation error method to identify the best model from the data. This finds b and a in
by creating a system of linear equations and solving them with the MATLAB® \ operator. Here A(w(k)) and B(w(k)) are the Fourier transforms of the polynomials a and b, respectively, at the frequency w(k), and n is the number of frequency points (the length of h and w). This algorithm is based on Levi . Several variants have been suggested in the literature, where the weighting function wt gives less attention to high frequencies.
The superior ("output-error") algorithm uses the damped Gauss-Newton method for iterative search , with the output of the first algorithm as the initial estimate. This solves the direct problem of minimizing the weighted sum of the squared error between the actual and the desired frequency response points.
 Levi, E.C., "Complex-Curve Fitting," IRE Trans. on Automatic Control, Vol.AC-4 (1959), pp.37-44.
 Dennis, J.E., Jr., and R.B. Schnabel, Numerical Methods for Unconstrained Optimization and Nonlinear Equations, Englewood Cliffs, NJ: Prentice-Hall, 1983.