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The best intuitive description of Laplace transform I've ever seen:

At first glance, it would appear that the strategy of the Laplace transform is the same as the Fourier transform: correlate the time domain signal with a set of basis functions to decompose the waveform. Not true! Even though the mathematics is much the same, the rationale behind the two techniques is very different.

The Laplace transform can be viewed as probing the system's impulse response with various exponentially decaying sinusoids. Probing waveforms that produce a cancellation are called poles and zeros.

This allows us instead of describing frequency response for every $\omega$ use a small set of feature points that determine the behavior of a system in all other points (including the part of $s$-plane $s=j\omega$ which is a frequency response).

There's a nice analogy for this in a book:

Now, think about how you understand the relationship between elevation and distance along the train route, compared to that of the conductor. Since you have directly measured the elevation along the way, you can rightly claim that you know everything about the relationship. In comparison, the conductor knows this same complete information, but in a simpler and more intuitive form: the location of the hills and valleys that cause the dips and humps along the path. While your description of the signal might consist of thousands of individual measurements, the conductor's description of the signal will contain only a few parameters.

The best intuitive description of Laplace transform I've ever seen.

The best intuitive description of Laplace transform I've ever seen:

At first glance, it would appear that the strategy of the Laplace transform is the same as the Fourier transform: correlate the time domain signal with a set of basis functions to decompose the waveform. Not true! Even though the mathematics is much the same, the rationale behind the two techniques is very different.

The Laplace transform can be viewed as probing the system's impulse response with various exponentially decaying sinusoids. Probing waveforms that produce a cancellation are called poles and zeros.

This allows us instead of describing frequency response for every $\omega$ use a small set of feature points that determine the behavior of a system in all other points (including the part of $s$-plane $s=j\omega$ which is a frequency response).

There's a nice analogy for this in a book:

Now, think about how you understand the relationship between elevation and distance along the train route, compared to that of the conductor. Since you have directly measured the elevation along the way, you can rightly claim that you know everything about the relationship. In comparison, the conductor knows this same complete information, but in a simpler and more intuitive form: the location of the hills and valleys that cause the dips and humps along the path. While your description of the signal might consist of thousands of individual measurements, the conductor's description of the signal will contain only a few parameters.

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The best intuitive description of Laplace transform I've ever seen.