Answers are grounded in this paper and cite their sources.
The azimuthal average throws away everything about a ring except its mean, including the information that distinguishes a true ring from an arc or a spot. This paper develops the complementary statistic, the azimuthal Fourier decomposition at fixed polar angle, and computes its discriminating power at the Cold Spot's latitude. A genuine ring places all its power in the zeroth azimuthal mode; a localised Gaussian spot of the Cold Spot's dimensions places only 0.059 of its azimuthal power there, spreading the rest over modes up to about m equals 17, with 0.941 of the power in modes one and above. An isotropic sky's rings, by contrast, return a zeroth-mode fraction averaging 0.103. The azimuthal spectrum thus separates the three cases, ring, spot, and ordinary sky, on a single ring's data, and it identifies the measurement that a future claim of ring structure must publish: not the average, but the mode fractions. The study is computed, not measured.
No takes yet. Share an insight, caveat, or question.
William Alexander Aldred (2026) studied this question.
Synapse has enriched 8 closely related papers on similar clinical questions. Consider them for comparative context: