Double Fourier sphere method
In mathematics, the double Fourier sphere (DFS) method is a technique that transforms a function defined on the surface of the sphere to a function defined on a rectangular domain while preserving periodicity in both the longitude and latitude directions.
Introduction
[edit ]First, a function {\displaystyle f(x,y,z)} on the sphere is written as {\displaystyle f(\lambda ,\theta )} using spherical coordinates, i.e.,
- {\displaystyle f(\lambda ,\theta )=f(\cos \lambda \sin \theta ,\sin \lambda \sin \theta ,\cos \theta ),(\lambda ,\theta )\in [-\pi ,\pi ]\times [0,\pi ].}
The function {\displaystyle f(\lambda ,\theta )} is {\displaystyle 2\pi }-periodic in {\displaystyle \lambda }, but not periodic in {\displaystyle \theta }. The periodicity in the latitude direction has been lost. To recover it, the function is "doubled up" and a related function on {\displaystyle [-\pi ,\pi ]\times [-\pi ,\pi ]} is defined as
- {\displaystyle {\tilde {f}}(\lambda ,\theta )={\begin{cases}g(\lambda +\pi ,\theta ),&(\lambda ,\theta )\in [-\pi ,0]\times [0,\pi ],\\h(\lambda ,\theta ),&(\lambda ,\theta )\in [0,\pi ]\times [0,\pi ],\\g(\lambda ,-\theta ),&(\lambda ,\theta )\in [0,\pi ]\times [-\pi ,0],\\h(\lambda +\pi ,-\theta ),&(\lambda ,\theta )\in [-\pi ,0]\times [-\pi ,0],\\\end{cases}}}
where {\displaystyle g(\lambda ,\theta )=f(\lambda -\pi ,\theta )} and {\displaystyle h(\lambda ,\theta )=f(\lambda ,\theta )} for {\displaystyle (\lambda ,\theta )\in [0,\pi ]\times [0,\pi ]}. The new function {\displaystyle {\tilde {f}}} is {\displaystyle 2\pi }-periodic in {\displaystyle \lambda } and {\displaystyle \theta }, and is constant along the lines {\displaystyle \theta =0} and {\displaystyle \theta =\pm \pi }, corresponding to the poles.
The function {\displaystyle {\tilde {f}}} can be expanded into a double Fourier series
- {\displaystyle {\tilde {f}}\approx \sum _{j=-n}^{n}\sum _{k=-n}^{n}a_{jk}e^{ij\theta }e^{ik\lambda }}
History
[edit ]The DFS method was proposed by Merilees[1] and developed further by Steven Orszag.[2] The DFS method has been the subject of relatively few investigations since (a notable exception is Fornberg's work),[3] perhaps due to the dominance of spherical harmonics expansions. Over the last fifteen years it has begun to be used for the computation of gravitational fields near black holes [4] and to novel space-time spectral analysis.[5]
References
[edit ]- ^ P. E. Merilees, The pseudospectral approximation applied to the shallow water equations on a sphere, Atmosphere, 11 (1973), pp. 13–20
- ^ S. A. Orszag, Fourier series on spheres, Mon. Wea. Rev., 102 (1974), pp. 56–75.
- ^ B. Fornberg, A pseudospectral approach for polar and spherical geometries, SIAM J. Sci. Comp, 16 (1995), pp. 1071–1081
- ^ R. Bartnik and A. Norton, Numerical methods for the Einstein equations in null quasispherical coordinates, SIAM J. Sci. Comp, 22 (2000), pp. 917–950
- ^ C. Sun, J. Li, F.-F. Jin, and F. Xie, Contrasting meridional structures of stratospheric and tropospheric planetary wave variability in the northern hemisphere, Tellus A, 66 (2014)
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