Geoscience Reference
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The half-wave mode, R S R N > 0 . In this case, an integer number of half-
waves lies on a field-lines. The resonance frequencies are
ω n
ω A
i γ n
= n
ω A ,
n =0 ,
±
1 ,
±
2 ,....
(5.20)
The relative decrement is independent of the harmonic number n and
γ n
ω A
1
2 π log ( R S R N ) .
=
(5.21)
The quarter-wave mode, R S R N < 0 . The field-lines length is 1 / 4 , 3 / 4 ,
5 / 4 ,... of the wavelength. The resonance frequencies are
ω n
ω A
1
2
i γ n
= n
ω A ,
n =0 ,
±
1 ,
±
2 ,
±
3 ,...
(5.22)
and the relative decrement is
γ n
ω A
1
2 π log
=
|
R S R N |
.
(5.23)
In the two limiting cases:
Σ P
1and Σ P
Small conductivities,
1, the decrement is
π Σ P
+ Σ P .
γ n
ω A
1
(5.24)
Σ P
1and Σ P
Large conductivities,
1 , the decrement is
1
Σ P
.
γ n
ω A
1
π
1
Σ P
+
(5.25)
Σ P =
Σ P =
Σ P ,and R = R S = R N =
In the symmetrical case at
1
Σ P / 1+ Σ P , we find from (5.21) that
π log
Σ P
1+ Σ P
γ n
ω A
1
1
ω A = πc A
l z
=
with
.
The dependence of the decrement γ n and the Q-factor Q n = ω A / 2 γ n of the
fundamental mode on Σ P are presented in Fig. 5.3. For dayside conditions at
moderate solar activity the normalized Σ P
10, and for nighttime conditions
Σ P
0 . 5. It can be seen from Fig. 5.3 that the Q-factor varies from 9 . 8at
the daytime to 1 . 4 at nighttime.
Below, we shall present fields expanded by eigenfunctions (5.12). However,
it is cumbersome to find a series the eigenfunctions of the generalized boundary
problem. We therefore prefer to regard (5.9)-(5.10) as a problem on wave
eigennumbers, keeping for it the designation of 'Dungey's problem'.
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