Polar Fourier Transform Calculator

Model radial data across frequency bins accurately. See coefficients, magnitude trends, and reconstruction indicators clearly. Download polished summaries for analysis, reporting, and quick validation.

Transform Results

This output uses a discrete approximation of the continuous polar Fourier integral.

Magnitude Heatmap

Frequency radius vs frequency angle

This line shows magnitude across frequency radii for one chosen frequency angle.

Coefficient Table

Real, imaginary, magnitude, phase, and power values
# ρ φ (deg) Real Imag Magnitude Phase (deg) Power

Calculator Inputs

Enter a polar signal grid, choose frequency coordinates, then calculate the transform.

Comma-separated radii. Example: 1,2,3
Comma-separated sample angles.
Applies to sample angles and frequency angles.
Target radial frequencies.
Target angular frequencies.
Multiplies every input amplitude before transforming.
Leave blank to use average radius spacing.
Use degrees or radians, matching your angle unit.
Controls table and summary formatting.
N equals radius count × angle count.
Applied along both radius and angle dimensions.
Enter one row per radius. Each row must contain the same number of values as the angle list.

Advanced options

Matrix mapping:
Row index → radius value.
Column index → angle value.
Cell value → signal amplitude at that polar coordinate.

Example Data Table

This sample matches the default matrix loaded in the calculator.

Radius 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

Formula Used

The continuous polar Fourier transform can be written as:

F(ρ, φ) = ∫00 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(θjn) · 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.

  • Magnitude: |F| = √(Real² + Imag²)
  • Phase: atan2(Imag, Real)
  • Power: |F|²

How to Use This Calculator

  1. Enter radius values in ascending order.
  2. Enter the angle list that matches each column in the matrix.
  3. Paste one matrix row for every radius value.
  4. Enter target frequency radii and target frequency angles.
  5. Choose angle units, normalization, and an optional window function.
  6. Keep the Jacobian option enabled for standard polar-area weighting.
  7. Press Calculate Transform to generate coefficients and plots.
  8. Export the coefficient table as CSV or PDF if needed.

FAQs

1) What does this calculator actually transform?

It transforms a signal sampled on a polar grid. Each matrix cell represents one amplitude measured at a radius and angle pair.

2) Why is the radial weight r important?

In polar coordinates, area elements scale with radius. Including r makes the discrete sum closer to the continuous polar integral.

3) When should I use a window function?

Use a window when your sampled grid is short or sharply truncated. It reduces leakage and smooths edge effects in the estimated spectrum.

4) What does the zero frequency radius mean?

A frequency radius of zero measures the overall low-frequency or average-like content of the input signal across the chosen angular directions.

5) Can I enter angles in radians?

Yes. Change the angle unit selector to radians, then enter both sample angles and frequency angles in radians.

6) Why must matrix rows and columns match the lists?

Every row maps to one radius, and every column maps to one angle. A mismatch breaks the coordinate mapping and invalidates the transform.

7) What does normalization change?

Normalization rescales coefficients. It does not move peaks, but it changes the numeric size of real, imaginary, magnitude, and power values.

8) Is this a continuous exact transform?

No. It is a numerical approximation based on finite sampled points, chosen frequency coordinates, spacing estimates, and selected preprocessing options.

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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.