I have a slowly varying sinusoidal system. The output is separated using methods that produce a real signal $x(t)$ and quadrature component $y(t)$ such that $x(t)$ represents the real physical value of the signal, $x^2 + y^2$ is instantaneous amplitude and $\mbox{atan}(y,x)$ is the instantaneous cosine argument with respect to a central frequency $\omega_c$. So you can think of it as $\omega_c + \phi(t)$ but those two pieces are bundled and the phase would have to be unwrapped to get at $\phi$.
I guess these qualities are unique enough to say that $z(t)=x+iy$ is the Analytic Signal representation of $x(t)$ for that frequency band and that $iy=\hat{x}$ is the Hilbert transform of $x$ in some bandpassed sense, but my knowledge is limited in this area.
Let's say this signal is the output of a linear and mostly time-invariant system with complex response $H(\omega)$. I am only interested in $H(\omega_c)$ at the widely spaced central frequencies and assume it is constant across the passed band around {\omega_c}. $H$ produces both amplitude and phase change but its characteristics are not known quantitatively. I can only probe it with the input and output I have, not probe it.
The idea I am exploring here is how to use the data I have to infer $H(\omega_c)$. If I take the complex output $Z$ as the Analytic Signal and input $W$ and do a complex regression $Z(\omega,t) \approx H(\omega) W(\omega,t) + \varepsilon(t)$ on the input using time to provide samples and yielding an estimate $\hat{H}$ is that an estimate of $H$? A good one? One concern I have is that $Z$ and $W$ likely have no negative frequency content, so I'm concerned that I'll be learning about the analytical analog of $H$ or something like that.