Model radial data across frequency bins accurately. See coefficients, magnitude trends, and reconstruction indicators clearly. Download polished summaries for analysis, reporting, and quick validation.
This output uses a discrete approximation of the continuous polar Fourier integral.
This line shows magnitude across frequency radii for one chosen frequency angle.
| # | ρ | φ (deg) | Real | Imag | Magnitude | Phase (deg) | Power |
|---|
This sample matches the default matrix loaded in the calculator.
| Radius | 0° | 45° | 90° | 135° | 180° | 225° | 270° | 315° |
|---|---|---|---|---|---|---|---|---|
| 1 | 5 | 7 | 9 | 7 | 5 | 3 | 1 | 3 |
| 2 | 6 | 9 | 12 | 9 | 6 | 3 | 2 | 3 |
| 3 | 7 | 11 | 15 | 11 | 7 | 4 | 2 | 4 |
The continuous polar Fourier transform can be written as:
F(ρ, φ) = ∫0∞ ∫02π f(r, θ)e-i2πρr cos(θ-φ) r dθ dr
This calculator uses a discrete approximation over sampled radii and angles:
F(ρm, φn) ≈ ΣΣ g(ri, θj) · e-i2πρmricos(θj-φn) · wi,j
Here, g(ri, θj) is the sampled amplitude, wi,j includes the selected window and spacing terms, and the optional Jacobian factor multiplies each sample by ri.
It transforms a signal sampled on a polar grid. Each matrix cell represents one amplitude measured at a radius and angle pair.
In polar coordinates, area elements scale with radius. Including r makes the discrete sum closer to the continuous polar integral.
Use a window when your sampled grid is short or sharply truncated. It reduces leakage and smooths edge effects in the estimated spectrum.
A frequency radius of zero measures the overall low-frequency or average-like content of the input signal across the chosen angular directions.
Yes. Change the angle unit selector to radians, then enter both sample angles and frequency angles in radians.
Every row maps to one radius, and every column maps to one angle. A mismatch breaks the coordinate mapping and invalidates the transform.
Normalization rescales coefficients. It does not move peaks, but it changes the numeric size of real, imaginary, magnitude, and power values.
No. It is a numerical approximation based on finite sampled points, chosen frequency coordinates, spacing estimates, and selected preprocessing options.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.