Use wave patterns adapted to a sphere
A plane has sinusoidal waves; a sphere has spherical harmonics . Higher degree gives finer patterns. Different values describe directional structure at that degree. The coefficients specify amplitudes and phases. After removing the mean and dipole we begin at degree two.
Complex harmonics are convenient, but temperature is real. Negative-index coefficients are fixed by conjugacy and cannot be independent complex draws. Each degree retains exactly twice the degree plus one independent real coordinates. An orthonormal real-harmonic basis gives the same count and calculation.
Estimate a theoretical mean from one realization
Statistical isotropy assigns the same theoretical variance to every independent real coordinate at a degree. In a Gaussian field, divide each coordinate by its standard deviation to obtain independent standard normal numbers. Their squared sum has a chi-square distribution with one degree of freedom per coordinate.
Power therefore scatters around its theoretical mean. At low degree the distribution is visibly skewed. Better instrumentation reduces measurement noise. The finite number of modes in this one sky still sets the remaining cosmic variance.
Reading: Lloyd Knox · Planck 2018 results. VI. Cosmological parameters
Calculate the scatter for large and small patterns
Degree two has five independent coordinates, giving fractional power scatter . Degree twenty has forty-one coordinates, giving . Higher-degree power still fluctuates, but concentrates more tightly across draws. These percentages describe power, not temperature amplitude.
The central ninety-five-percent sampling band at degree two is ; at degree twenty it is approximately . The low-degree interval is strongly asymmetric. A symmetric mean-plus-or-minus-standard-deviation band misses that shape.
Power also discards some map information. Changing positive-order coefficient phases while preserving real-field conjugacy rearranges hot and cold patches. If the squared sum at each degree stays fixed, so does angular power. Many different maps can share the same spectrum.
Two interval questions need different endpoints
With known theoretical power, ask where repeated estimates fall. Let be a chi-square quantile. Multiplying theoretical power by the lower and upper quantiles and dividing by the mode count gives a central ninety-five-percent sampling range.
With an observed estimate and unknown theoretical power, solve the same probability statement for the parameter instead. This produces a frequentist confidence interval: across repeated experiments, the constructed intervals cover the true power at the stated rate. Its endpoints differ from the sampling band. A Bayesian posterior interval depends jointly on the likelihood and the chosen prior.
Reading: Lloyd Knox · Planck 2018 results. VI. Cosmological parameters
Smoothing cannot create another independent sky
An ideal circular Gaussian beam multiplies each degree’s coefficients by a fixed window. Power falls by its square, but the number of independent coordinates stays the same. If the theory is smoothed consistently, fractional cosmic variance remains set by mode count. Real observations also add noise and masks, treated next.
This generator stops at degree twenty-four and uses a prescribed teaching spectrum. It illustrates mode counting and sampling scatter, with no acoustic peaks or observed Planck map. The separate acoustic-grid experiment studies the high-degree peak structure.