Geoscience Reference
In-Depth Information
x t
x r
1
2
k A
1.5
0.8
1
Initial wave
0.6
0.5
0.4
0
c A
0.2
0.5
0
−1
0
5
10
15
20
0
5
10
15
20
x
x
20 x 10 3
4
b y /B 0
3
b || /B 0
15
2
b x /B 0
10
1
5
0
0
−1
−2
5
0
5
10
15
20
0
5
10
15
20
x
x
Fig. 4.3. Left top frame: the Alfven velocity (solid line) and Alfven wave number
(dashed line) as a function of x .Righttopframe:Effectivepotential U ( x ) . The
initial wave propagates from left to right, from the region with low Alfven velocity
to high velocity. Two vertical dotted lines show the location of the turning point
( x t ) and resonance point ( x r ) . Left bottom: wave magnetic field near a resonance
surface. Right bottom: Energy flux to resonance surfaces
it. The incidence of an H -polarized wave onto a layered medium has been
considered and solved completely in ([7], [8]).
The qualitative pattern of the fields can be obtained if we wr ite (4.5 3) in
the form of the Schrodinger wave equation. Substitution b = u k A
k 2
into
(4.53) gives
d 2 u ( x )
dx 2
U ( x ) u ( x )=0 ,
(4.54)
where
dk A
dx
2
d 2 k A
dx 2
1
2
1
k A
+ 3
4
1
k A
U = k y + k 2
k A
2 .
k 2
k 2
The left top panel of Fig. 4.3 presents the Alfven velocity c A ( x )and
wavenumber k A ( x ). Dependence of the effective potential U ( x ) on the transver-
sal coordinate x is shown in the right top panel. The coordinate x and k A ( x )
are normalized on a scale l / 2 . The function U ( x ) is calculated at frequency
 
Search WWH ::




Custom Search