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A surface harmonic of degree
(where
is a non-negative integer), denoted
, is defined as a well-behaved solution
to
![$\displaystyle r^{\,2}\,\nabla^{\,2} {\cal S}_n + n\,(n+1)\,{\cal S}_n = 0$](img4310.png) |
(12.36) |
on the surface of a sphere (i.e.,
constant). Here,
,
,
are standard spherical coordinates, and
is the Laplacian operator. It follows that (Love 1927)
![$\displaystyle {\cal S}_n(\theta,\varphi) = \sum_{m=0,n} \left[c_n^{\,m}\,P_n^{\...
...\,\cos(m\,\varphi) + d_n^{\,m}\,P_n^{\,m}(\cos\theta)\,\sin(m\,\varphi)\right],$](img4313.png) |
(12.37) |
where the
and
are arbitrary coefficients, and the
associated Legendre functions.
A solid harmonic of degree
(where
is a non-negative integer), denoted
, is defined as a well-behaved solution
to
![$\displaystyle \nabla^{\,2} {\cal R}_n = 0$](img4318.png) |
(12.38) |
in the interior of a sphere (i.e., the region
constant). It follows that (Love 1927)
![$\displaystyle {\cal R}_n(r,\theta,\varphi) \propto r^{\,n}\,{\cal S}_n(\theta,\varphi).$](img4320.png) |
(12.39) |
In particular, the functions
and
, introduced in Section 12.3,
are solid harmonics of degree
. Note that the Cartesian coordinates
(where
runs from
to
) are solid
harmonics of degree
. Moreover,
is a solid harmonic of degree
. Finally,
,
specified in Equation (12.35), is a solid harmonic of degree 2.
The following results regarding solid harmonics are useful (Love 1927):
Here, use has been made of the Einstein summation convention (Riley 1974).
Next: Planetary Rotation
Up: Terrestrial Ocean Tides
Previous: Expansion of Tide Generating
Richard Fitzpatrick
2016-01-22