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50
40
30
∝Im b
ϕ
20
∝
Re b
ϕ
10
0
−10
−20
∝Re E
ν
−30
∝Im E
ν
−
40
−50
0
0.2
0.4
0.6
0.8
cos
θ
Fig. 6.9.
Field line distribution of the real and imaginary parts of the electric and
magnetic components of the 2-nd FLR-harmonics at field line
L
= 3 as a function
of colatitude
θ.
Point cos
θ
= 0 is the equatorial point and cos
θ
=0
.
8 is the pierce
point of the field line in the ionosphere
field varies significantly at heights about 200 km and it changes its sign at
h
≈
300 km. The relative growth of the electric field in the ionosphere results
in increasing Joule dissipation and decrement.
The same dependencies for the 2-nd harmonic at the shell
L
=3are
shown in Fig. 6.9. Note that the azimuthal component of the magnetic field
b
ϕ
(
x
)
e
1
(
x
) varies rapidly in the ionospheric
E
-layer. It grows from zero
under the ionosphere to the maximal value above the ionosphere. On the other
hand, the component
E
ν
(
x
)
∝
e
2
(
x
) is almost constant in the
E
-layer.
In the above calculations the ionospheric parameters typical for the solar
maximum are used.
∝
Meridional Distribution of the FLR-Amplitudes and Phases
The meridional distribution of the FLR-amplitude and phase above the
ionosphere are determined by (6.88), (6.89) and (6.90). In order to utilize their
we need to define FLR-periods, half-widths, and coecients
C
0
and
Λ
0
. Res-
onance period and half-width of the FLR are determined from the dispersion
equation (6.121).
C
0
and
Λ
0
are given by (6.111)-(6.116). The calculations
have been carried out at
Σ
P
=0
.
8
10
8
km/s. The equatorial distribution of
the ion concentration has been taken from Fig. 6.3 (curve 2) with plasmapause
at
L
pp
=3
.
9 that corresponds to a mean value of the plasmapause position
at
K
p
= 5. The calculations are performed for
m
= 1. Results of the calcu-
lations are shown in Fig. 6.10. Panels (a) and (b) show dependencies of the
FLR-period and half-width against
L
-shell, and (c) and (d) show abs
C
0
(
L
)
and abs
Λ
0
(
L
).
Let us now find the meridional distribution of the wave field produced by
a driver of period
T
. From 6.10a follows that there are two fundamentally
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