For constant Electron density, common path length , and a solenoidal isotropic spectral tensor, the rotation-measure correlation contains the window . As becomes large compared with the correlation length, this window acts as within the integral. The transverse projector then has component one, yielding the displayed two-dimensional Fourier transform. For finite , the windowed integral retains longitudinal modes and endpoint corrections. The method of using such rotation measure correlations to infer magnetic spectra is developed by Enßlin and Vogt.
Invert the two-dimensional Fourier transform in the long-path projection of a magnetic correlation, then perform the angular integration in polar coordinates. The angular integral is , a Bessel function of the first kind, giving the displayed Hankel transform with the stated Fourier-Hankel normalization for an isotropic spectrum. The result recovers the scalar tensor coefficient , whose shell-integrated magnetic energy spectrum has an additional factor .
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