Geoscience Reference
In-Depth Information
this current corresponds to negative current moment. In our study the
CG current
moment is positive since we use the upward directed vertical axis
z
,asshown
in Fig.
4.1
.
Let R
e
and R
i
D
R
e
C
d be the radii of the Earth and the ionosphere, where d is
the height of the non-conductive atmosphere. The upward-directed lumped element
m
situated in the atmosphere has the coordinates r
D
R and
D
0 as shown in
Fig.
4.1
. In such a case the Fourier transform of the current density j
s
produced by
the lumped source can be written as follows:
m.!/
2r
2
sin
ı.r
R/ı./;
j
s
.r;;!/
D
(4.9)
where ı.x/ is the so-called Dirac's function/delta-function, which equals zero for
all the x, except for x
D
0, and by definition
Z
ı.x/dx
D
1:
(4.10)
1
The arrangement of the formula (
4.9
)forj
s
is in accord with the requirement that
the integral of j
s
over the space gives the total current moment m.!/. Indeed, the
elementary current moment is j
s
dV, where dV
D
r
2
sin dd'dr is the volume
element/differential in the spherical coordinates. Multiplying Eq. (
4.9
)bydV and
integrating the elementary current moment over the whole space yields the value
m.!/, which is required to be proved.
Substituting Eq. (
4.9
)forj
s
into Eq. (
4.8
) gives a differential equation which
contains the delta-function. In order to derive a boundary condition at point r
D
R
one should integrate Eq. (
4.8
) over r between R
Ǜ and R
C
Ǜ, and then formally
take Ǜ
!
0. Taking into account the continuity of U at r
D
R , we thus obtain the
following condition at r
D
R
m.!/ı./
2i"
0
!R
2
sin
;
Œ@
r
.rU/
D
(4.11)
where the square bracket denotes the jump of the function, that is, Œf .x/
D
f .x
C
0/
f .x
0/.InEq.(
4.11
) the square bracket stands for the jump of the
function @
r
.rU/ at r
D
R.
Boundary conditions (
4.11
) may be simplified because the point current element
occurs at the small altitude above the ground, that is, in the case R
R
e
d.
If the Earth is supposed to be a perfect conductor, the tangential component of the
electric field E
becomes zero at the terrestrial surface. Whence it follows from
Eq. (
4.7
) that @
r
.rU/
D
0 at r
D
R
e
. Combining this condition with Eq. (
4.11
)
in the extreme limit case R
!
R
e
we come to the following boundary condition
at r
D
R
e
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