In mathematics, vector spherical harmonics (VSH) are an extension of the scalar spherical harmonics for use with vector fields. The components of the VSH are complex-valued functions expressed in the spherical coordinate basis vectors.
DefinitionEditMain PropertiesEditSymmetryEdit
Like the scalar spherical harmonics, the VSH satisfy

which cuts the number of independent functions roughly in half. The star indicates complex conjugation.
OrthogonalityEdit
The VSH are orthogonal in the usual three-dimensional way at each point
:

They are also orthogonal in Hilbert space:

An additional result at a single point
(not reported in Barrera et al, 1985) is, for all
,

Vector multipole momentsEdit
The orthogonality relations allow one to compute the spherical multipole moments of a vector field as

The gradient of a scalar fieldEdit
Given the multipole expansion of a scalar field

we can express its gradient in terms of the VSH as

DivergenceEdit
For any multipole field we have

By superposition we obtain the divergence of any vector field:

We see that the component on Φlm is always solenoidal.
CurlEdit
For any multipole field we have

By superposition we obtain the curl of any vector field:

LaplacianEdit
The action of the Laplace operator
separates as follows:

where
and

Also note that this action becomes symmetric, i.e. the off-diagonal coefficients are equal to
, for properly normalized VSH.
ExamplesEditFirst vector spherical harmonicsEdit
.

.



.



Expressions for negative values of m are obtained by applying the symmetry relations.
ApplicationsEditElectrodynamicsEdit
The VSH are especially useful in the study of multipole radiation fields. For instance, a magnetic multipole is due to an oscillating current with angular frequency
and complex amplitude

and the corresponding electric and magnetic fields, can be written as

Substituting into Maxwell equations, Gauss' law is automatically satisfied

while Faraday's law decouples as

Gauss' law for the magnetic field implies

and Ampère-Maxwell's equation gives

In this way, the partial differential equations have been transformed into a set of ordinary differential equations.
Alternative definitionEdit

Angular part of magnetic and electric vector spherical harmonics. Red and green arrows show the direction of the field. Generating scalar functions are also presented, only the first three orders are shown (dipoles, quadrupoles, octupoles).
In many applications, vector spherical harmonics are defined as fundamental set of the solutions of vector Helmholtz equation in spherical coordinates.[6][7]
In this case, vector spherical harmonics are generated by scalar functions, which are solutions of scalar Helmholtz equation with the wavevector
.

here
- associated Legendre polynomials, and
- any of spherical Bessel functions.
Vector spherical harmonics are defined as:
- longitual harmonics
- magnetic harmonics
- electric harmonics
Here we use harmonics real-valued angular part, where
, but complex functions can be introduced in the same way .
Let us introduce the notation
. In the component form vector spherical harmonics are written as:


![{\displaystyle {\begin{aligned}{\mathbf {N} _{emn}(k,\mathbf {r} )={\frac {z_{n}(\rho )}{\rho }}\cos(m\varphi )n(n+1)P_{n}^{m}(\cos(\theta ))\mathbf {e} _{\mathbf {r} }+}\\{+\cos(m\varphi ){\frac {dP_{n}^{m}(\cos(\theta ))}{d\theta }}}{\frac {1}{\rho }}{\frac {d}{d\rho }}\left[\rho z_{n}(\rho )\right]\mathbf {e} _{\theta }-\\{-m\sin(m\varphi ){\frac {P_{n}^{m}(\cos(\theta ))}{\sin(\theta )}}}{\frac {1}{\rho }}{\frac {d}{d\rho }}\left[\rho z_{n}(\rho )\right]\mathbf {e} _{\varphi }\end{aligned}}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/7ad38d781b484c1a1b550920518d596c88de2c37)
![{\displaystyle {\begin{aligned}\mathbf {N} _{omn}&(k,\mathbf {r} )={\frac {z_{n}(\rho )}{\rho }}\sin(m\varphi )n(n+1)P_{n}^{m}(\cos(\theta ))\mathbf {e} _{\mathbf {r} }+\\&+\sin(m\varphi ){\frac {dP_{n}^{m}(\cos(\theta ))}{d\theta }}{\frac {1}{\rho }}{\frac {d}{d\rho }}\left[\rho z_{n}(\rho )\right]\mathbf {e} _{\theta }+\\&+{m\cos(m\varphi ){\frac {P_{n}^{m}(\cos(\theta ))}{\sin(\theta )}}}{\frac {1}{\rho }}{\frac {d}{d\rho }}\left[\rho z_{n}(\rho )\right]\mathbf {e} _{\varphi }\end{aligned}}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/4528c43603f7c5868f920afcbdae5bec0d6f1af3)
There is no radial part for magnetic harmonics. For electric harmonics, the radial part decreases faster than angular, and for big
can be neglected. We can also see that for electric and magnetic harmonics angular parts are the same up to permutation of the polar and azimuthal unit vectors, so for big
electric and magnetic harmonics vectors are equal in value and perpendicular to each other.
Longitual harmonics:

OrthogonalityEdit
The solutions of the Helmholtz vector equation obey the following orthogonality relations:[7]
![{\displaystyle {\int _{0}^{2\pi }\int _{0}^{\pi }\mathbf {L} _{^{e}_{o}mn}\cdot \mathbf {L} _{^{e}_{o}mn}\sin \vartheta d\vartheta d\varphi }{=(1+\delta _{m,0}){\frac {2\pi }{(2n+1)^{2}}}{\frac {(n+m)!}{(n-m)!}}k^{2}\left\{n\left[z_{n-1}(kr)\right]^{2}+(n+1)\left[z_{n+1}(kr)\right]^{2}\right\}}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/3caf9a3a862e813514a86ae833494cfd4f0f9c8a)
![{\displaystyle {\int _{0}^{2\pi }\int _{0}^{\pi }\mathbf {M} _{^{e}_{o}mn}\cdot \mathbf {M} _{^{e}_{o}mn}\sin \vartheta d\vartheta d\varphi }{=(1+\delta _{m,0}){\frac {2\pi }{2n+1}}{\frac {(n+m)!}{(n-m)!}}n(n+1)\left[z_{n}(kr)\right]^{2}}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/61acd92c5fd19ad05b94d6e9792241b6dc468972)
![{\displaystyle \int _{0}^{2\pi }\int _{0}^{\pi }\mathbf {N} _{^{e}_{o}mn}\cdot \mathbf {N} _{^{e}_{o}mn}\sin \vartheta d\vartheta d\varphi }{=(1+\delta _{m,0}){\frac {2\pi }{(2n+1)^{2}}}{\frac {(n+m)!}{(n-m)!}}n(n+1)\left\{(n+1)\left[z_{n-1}(kr)\right]^{2}+n\left[z_{n+1}(kr)\right]^{2}\right\}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/6304776dd0142be5974ab4f30dd4b895cc093fb0)
![{\displaystyle {\int _{0}^{\pi }\int _{0}^{2\pi }\mathbf {L} _{^{e}_{o}mn}\cdot \mathbf {N} _{^{e}_{o}mn}\sin \vartheta d\vartheta d\varphi }{=(1+\delta _{m,0}){\frac {2\pi }{(2n+1)^{2}}}{\frac {(n+m)!}{(n-m)!}}n(n+1)k\left\{\left[z_{n-1}(kr)\right]^{2}-\left[z_{n+1}(kr)\right]^{2}\right\}}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/550cfe2b979c59738bfb9c3213cc844a29dad4dd)
All other integrals over the angles between different functions or functions with different indices are equal to zero.
Rotation and inversionEdit

Illustration of the transformation of vector spherical harmonics under rotations. One can see that they are transformed in the same way as the corresponding scalar functions.
Under rotation, vector spherical harmonics are transformed through each other in the same way as the corresponding scalar spherical functions, which are generating for a specific type of vector harmonics. For example, if the generating functions are the usual spherical harmonics, then the vector harmonics will also be transformed through the Wigner D-matrixes[8][9][10]
![{\displaystyle {\hat {D}}(\alpha ,\beta ,\gamma )\mathbf {Y} _{JM}^{(s)}(\theta ,\varphi )=\sum _{m'=-\ell }^{\ell }[D_{MM'}^{(\ell )}(\alpha ,\beta ,\gamma )]^{*}\mathbf {Y} _{JM'}^{(s)}(\theta ,\varphi ),}](https://wikimedia.org/api/rest_v1/media/math/render/svg/c8058dc6bc3db6f74f9347479626e2a3aca7673b)
The behavior under rotations is the same for electrical, magnetic and longitudinal harmonics.
Under inversion, electric and longitudinal spherical harmonics behave in the same way as scalar spherical functions, i.e.

and magnetic ones have the opposite parity:

Fluid dynamicsEdit
In the calculation of the Stokes' law for the drag that a viscous fluid exerts on a small spherical particle, the velocity distribution obeys Navier-Stokes equations neglecting inertia, i.e.,

with the boundary conditions

where U is the relative velocity of the particle to the fluid far from the particle. In spherical coordinates this velocity at infinity can be written as

The last expression suggests an expansion in spherical harmonics for the liquid velocity and the pressure
-
Substitution in the Navier–Stokes equations produces a set of ordinary differential equations for the coefficients.
Integral relationsEditwhere
, index
means, that spherical hankel functions are used.