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Three ways to solve the Poisson equation on a sphere with Gaussian forcing

✍ Scribed by John P. Boyd; Cheng Zhou


Publisher
Elsevier Science
Year
2009
Tongue
English
Weight
749 KB
Volume
228
Category
Article
ISSN
0021-9991

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✦ Synopsis


Motivated by the needs of vortex methods, we describe three different exact or approximate solutions to the Poisson equation on the surface of a sphere when the forcing is a Gaussian of the three-dimensional distance, r 2 w ΒΌ expðÀ2 2 Γ°1 Γ€ cosΓ°hÞÞ Γ€ C Gauss ðÞ. (More precisely, the forcing is a Gaussian minus the ''Gauss constraint constant", C Gauss ; this subtraction is necessary because w is bounded, for any type of forcing, only if the integral of the forcing over the sphere is zero [Y. Kimura, H. Okamoto, Vortex on a sphere, J. Phys. Soc. Jpn. 56 (1987) 4203-4206; D.G. Dritschel, Contour dynamics/surgery on the sphere, J. Comput. Phys. 79 (1988) 477-483]. The Legendre polynomial series is simple and yields the exact value of the Gauss constraint constant, but converges slowly for large . The analytic solution involves nothing more exotic than the exponential integral, but all four terms are singular at one or the other pole, cancelling in pairs so that w is everywhere nice. The method of matched asymptotic expansions yields simpler, uniformly valid approximations as series of inverse even powers of that converge very rapidly for the large values of Γ° > 40Þ appropriate for geophysical vortex computations. The series converges to a nonzero OΓ°expðÀ4 2 ÞÞ error everywhere except at the south pole where it diverges linearly with order instead of the usual factorial order.


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