Treat the boundary data as -periodic in the angular variable. Denote the outer data by , and set for the inner data. Define their mean and nonconstant Fourier coefficients by
The outer data have reflection symmetry, so all their sine Fourier coefficients vanish. Their mean is , and their cosine Fourier coefficients are
The angular Fourier harmonics for a single-valued harmonic function in an annulus are and , with integer . Their radial factors are independent combinations of and ; the zero angular mode has radial factor . For arbitrary inner data, the sine and cosine modes need independent radial coefficients: forcing them to share one radial factor, as in the product form supplied in the paper, would impose an extra restriction. For either sine or cosine mode, if its outer and inner coefficients are and , the radial coefficients obey
Solving this linear system gives
It is convenient to collect the result into the annular harmonic interpolation factors
They satisfy , , and . The zero mode satisfies and . Therefore the required separation of variables solution is
All dependence on is given by the displayed integrals. Substituting leaves its Fourier series, and substituting leaves
the Fourier series of the specified outer step. The radial factors satisfy , so each nonconstant term satisfies Laplace's equation; and do also. For integrable boundary data the radial factors give exponential decay on every closed subannulus strictly inside , justifying the necessary termwise partial derivatives there.
There is a qualification at the two outer jump discontinuities. By pointwise convergence of a piecewise smooth Fourier series, the outer series gives at , whereas the printed data assign at those two points. Thus the displayed solution attains the outer data at their continuity points, and has radial limit at the jumps. One may separately assign the boundary value at the two exceptional points without changing the interior harmonic function, but no continuous extension can match the discontinuous data there. For piecewise smooth inner data, the analogous boundary trace agrees with at continuity points and with its midpoint at jumps. Some regularity of is necessary for a classical interpretation; the problem imposes none explicitly.

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