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10 24 g/ cm 3 . Then from (6.102) we have
mass m p =1 . 673
×
166 . 5
106
n 1 / 2
ω A ( L )=
1 . 015 /L ) 1 / 2 ,
=
L 4 ,
n 1 / 2
L 4 (1
e
e
atanh 0 . 889 n 1 / 2
e
,
1 . 015 /L ) 1 / 2 L 3
γ j ( L )= 0 . 637
j
(1
1
X
4
3 . 047 /L
94 . 19
LΩX
w 0
1+3 w 0
q =
.
(6.103)
If the frequencies ω A ( L ) and decrements γ L are found, one can determine the
FLR-half-width δ ( j )
L
in the magnetosphere if we take hold of (6.83) in the form
γ j
ω j ( L ) ,
δ ( j )
L
(6.104)
where ω j ( L )= j /dL . Mapping δ ( j L onto the ionosphere, one can express
the half-width of the resonance region δ ( j )
i
at the ionospheric height in terms
of δ ( j )
L
6523
L (4 L
δ ( j )
i
3) δ ( j L (km) .
(6.105)
Since the decrement is small, then from (6.103) follows that
d ln ( ω j ( L ))
dL
4
L +
1
2 L ( L
p
2 L .
≈−
1) +
(6.106)
From (6.105) and (6.106), we obtain for the half-width δ ( j )
L
outside the plas-
masphere:
γ j L
γ j L
3
δ ( j )
L
1) + p/ 2
.
4+1 / 2( L
Distribution of the Wave Fields
A field line distribution of the magnetic disturbances is given by e j ( w ) . Let
e j ( w ) be normalized by conditions
w 0
w 0
ν j c 2
2
ν 2
j
e 1 ( w )d w
e 2 ( w )d w =1 .
(6.107)
−w 0
−w 0
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