Laplace transform

Given a complex-valued function f(t) with tR, the Laplace transform is a function F:ΩCC such that every F(s) represents the weight of the function est in the decomposition

f(t)=12πi(+F(c+0.1i)e(c+0.1i)t+F(c+0.2i)e(c+0.2i)t++F(s)est+)==12πilimTciTc+iTestF(s)ds

for any c inside the Region of Convergence (ROC) — the set of sC for which the forward transform converges.

Bilateral vs. unilateral. The formulas above describe the bilateral Laplace transform, where F(s)=f(t)estdt and the ROC is a vertical strip σ1<Re(s)<σ2. The more common unilateral transform integrates from 0 to , with ROC a right half-plane Re(s)>σc.

A particular case would be the Fourier transform, whose picture corresponds to the case c=0 (provided c=0 lies in the ROC).

Both transformations have to do with the fact that some spaces of functions are Hilbert spaces, so we have a "basis". The original function can be thought as expressed in the Dirac delta basis, and the Fourier transform and Laplace transform are nothing but the expression of the same function in a different basis. See Fourier, Laplace and Dirichlet relationship.

What basis?, the natural for the generator of the translations.

Why a 1D Line Integral instead of CF(s)estds?

  1. Dimensionality: Since f(t) is a 1D function of time (tR), it requires a 1D continuum of basis elements to represent it.

  2. Linear Independence: Fixing Re(s)=c yields s=c+iω, giving a single degree of freedom ωR. The family {e(c+iω)t}ωR forms an orthogonal basis for ectf(t).

  3. Overcompleteness: The set of all exponentials {est}sC across the entire 2D complex plane is massively redundant (overcomplete). Integrating over all of C would sum infinitely many duplicate reconstructions of f(t) together, causing the surface integral to diverge.

  4. Analyticity: By Cauchy's Integral Theorem, every vertical line c within the ROC carries 100% of the information needed to reconstruct f(t). Shifting c changes the damping factor ect, but yields the exact same signal.

One Laplace transform or several ones?

It may seems that we have a Laplace transform for each c. But we have only one complex variable function F(s), with sC. When you calculate the (bilateral) Laplace transform of f(t), c does not exist in the formula:

L{f(t)}(s)=F(s)=f(t)estdt

(The unilateral version integrates from 0 to and is often denoted L{f(t)}(s)=0f(t)estdt.)
We can think that since

f(t)=12πicic+iF(s)estds

we have, indeed, different real-valued functions, a 1D restriction of F(s) along the line Re(s)=c:

Fc(ω):=F(c+iω)$$Butthen$Fc(ω)$isliterallythe1DFourierTransformofadifferentfunction:$ectf(t)$.Ineffect,$$Fc(ω)=F{ectf(t)}(ω)

since

ectf(t)=ect12πicic+iF(s)estds=ect12πiFc(ω)e(c+iω)tdω=12πiFc(ω)eiωtdω

Each "different" Laplace transform is, indeed, a Fourier transform of a "modified" function. And all these 1D slices Fc(ω) are rigidly bound to one another:

My interpretation

We can think of Laplace transform F(s) of f(t) as a kind of recipe to construct f(t) from exponential functions {est:sC}. But we don't need the whole F, we can fix a vertical line in C, Lc={c+iω:ωR},cR. Consider the s-plane as a collection of all the exponential functions. We can reconstruct f from the exponentials living in any of those lines

f(t)=12πic1ic1+iF(s)estds=12πic2ic2+iF(s)estds=

Example

This figure illustrates how a single complex landscape F(s)=1si unifies an infinite family of 1D Fourier transforms for the causal signal f(t)=eitu(t). (Here u(t) is the Heaviside step function, for issues of convergence)
Pasted image 20260803163409.png
For any vertical line s=c+iω within the Region of Convergence (c>0), the 1D cross-section Fc(ω) is literally the continuous Fourier transform of the exponentially damped signal ectf(t). As c decreases from 0.50 down to 0.05, the damping weakens: the smooth slices of the real part Re[Fc(ω)] grow taller (height 1/c) and narrower while maintaining a constant area of π. On the boundary c=0, the damping vanishes entirely, and this real part collapses into the Dirac delta distribution πδ(ω1)matching the real part of the Fourier transform of the causal tone eitu(t). Because all these 1D slices are rigidly bound together across the 2D surface F(s), reconstructing the original signal f(t) via the inverse Laplace transform along any vertical path Lc with c>0 yields the exact same underlying function.


Related: non homogeneous linear differential equations using Laplace
Related: Mellin transform.