Geoscience Reference
In-Depth Information
m.!/ı./
2i" 0 !R e sin :
@ r .rU/ D
(4.12)
Similarly, if the ionosphere is supposed to be a perfect conductor, the tangential
component of the electric field E becomes zero at the boundary with the iono-
sphere. Whence it follows from Eq. ( 4.7 ) the boundary condition at r D R i :
@ r .rU/ D 0:
(4.13)
4.1.3
Solution of the Problem
Finally, we have arrived at the second order differential Eq. ( 4.8 ), where the right-
hand side is equal to zero. This equation for the unknown potential function U
should be supplemented by two boundary conditions of Eqs. ( 4.12 ) and ( 4.13 ).
In standard mathematical technique, it is recommended to seek for the solution of
Eq. ( 4.8 )intheform
n A n h .1 n .kr/ C B n h .2 n .kr/ o P n .cos /;
X
U D
(4.14)
n
D
0
where A n and B n are the undetermined coefficients, h .1 n .x/ and h .2 n .x/ are the
spherical Bessel functions of the third kind, and P n .x/ stands for Legendre poly-
nomials. The definitions of these functions are found in Appendix A. To construct
the solution of the problem, the boundary condition ( 4.12 ) can be expanded in a
series of the Legendre polynomials. The representation of the delta-function ı./
through Legendre polynomials is given by Eqs. ( 4.59 ) and ( 4.60 ). Combining these
equations with Eq. ( 4.12 ), we come to the following boundary condition at r D R e
n C
P n .cos /:
X
m.!/
2i" 0 !R e
1
2
@ r .rU/ D
(4.15)
nD0
Substituting Eq. ( 4.14 )forU into Eqs. ( 4.13 ) and ( 4.15 ) we get the boundary
condition expanded in a series of the Legendre polynomials. This representation
of the boundary conditions gives a set of equations for undetermined coefficients
A n and B n
A n u . 1 n .kR i / C B n u . 2 n .kR i / D 0;
(4.16)
n C
:
m.!/
2i" 0 !R e
1
2
A n u .1 n .kR e / C B n u .2 n .kR e / D
(4.17)
 
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