I have seen different types of filters, and different slope values at -20 db, -40, etc.
The literature says that the order define the slope, but how? How can it be mathematically justified?
For example, I have a transfer function with a simple real pole \$H(s)=\frac{1}{1+\frac{s}{\omega_{0}}}\$ using \$j\omega\$ instead of \$s\$ \$H(j\omega)=\frac{1}{1+j\frac{\omega}{\omega_{0}}}\$ then the magnitude is:
$$ |H(j\omega)|=\left|\frac{1}{1+j\frac{\omega}{\omega_{0}}}\right|=\frac{1}{\sqrt{1^{2}+(\frac{\omega}{\omega_{0}})^{2}}} $$
$$H(j\omega)|_{dB}=20log_{10}(\frac{1}{\sqrt{1+(\frac{\omega}{\omega_{0}})^{2}}})$$
Next, I understand there are three cases:\$\omega<<\omega_{0}\$ , \$\omega>>\omega_{0}\$ and \$\omega=\omega_{0}\$. Lets say, working when the frequency is the same as the cutoff frequency, the magnitude and angle are
$$|H(j\omega_{0})|_{dB}=20log_{10}(\frac{1}{\sqrt{1+(\frac{\omega}{\omega_{0}})^{2}}})=$$
$$20log_{10}(\frac{1}{\sqrt{2}})\approx-3\:dB$$
$$\angle H(j\omega)=-arctan(1)=-\deg{45}=-\frac{\pi}{4}\,rad$$
This results in a piecewise linear asymptotic Bode plot for magnitude from 0 dB until the cutoff frequency and then drops at 20 dB per decade (the famous -20 dB/decade.)
How are these modified to -40 or -60 dB?
This is the case for a simple real pole. How does it work with a real zero,a pole/zero at the origin,complex conjugate zero/poles, etc?
How does it work in the other two cases of the simple real pole?