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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