Geoscience Reference
In-Depth Information
This equation holds true if
1
r
@
'
‰; and A
'
D
@
r
‰:
A
r
D
(5.93)
Finally we arrive at the following representation
A
D
O
r
r
@
'
‰
O'
@
r
‰
CO
z
A;
(5.94)
where
O
r
,
O'
, and
O
z
stand for the unit vectors. Substituting Eq. (
5.94
)for
A
into
Eq. (
5.73
) yields
1
r
@
'
A
z
@
z
A
'
D
1
r
@
'
A
C
@
r
z
‰;
ıB
r
D
(5.95)
1
r
@
z
'
‰
@
r
A;
ıB
'
D
@
z
A
r
@
r
A
z
D
(5.96)
r
@
r
rA
'
1
1
r
@
'
A
r
D
1
r
@
r
.r@
r
‰/
1
r
2
@
''
‰:
ıB
z
D
(5.97)
Similarly, substituting Eq. (
5.94
)for
A
into Eq. (
5.74
) yields
i!
r
@
'
‰;
E
r
D
@
r
dž
C
(5.98)
1
r
@
'
dž
i!@
r
‰;
E
'
D
(5.99)
E
z
D
@
z
dž
C
i!A:
(5.100)
Here, as we have noted above, the terms depending on the potentials dž and A
describe the shear Alfvén mode, whereas the terms depending on the potential ‰
correspond to the compressional mode.
Appendix D: Solutions of the Boundary Problems
Solution of the Problem Associated with IAR
In the magnetosphere .
z
>L/ the solution of wave equations for the potentials dž
and ‰ is given by Eqs. (
5.15
) and (
5.16
). Inside the IAR region .0<
z
<L/ the
solution of Eq. (
5.12
) describing Alfvén waves can be written as
dž
D
dž.0/ cos
!
z
V
AI
C
C
3
sin
!
z
;
(5.101)
V
AI
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