Geoscience Reference
In-Depth Information
Perturbations of hydrodynamic variables
ρ
1
,
u
and electromagnetic field
components
E
E
⊥
,E
and
b
b
⊥
,b
are expressed in terms of displace-
ment
ξ
as
b
B
0
ρ
1
ρ
0
b
B
0
=
∂
ξ
⊥
∂z
−
∇
·
ξ
,
,
−
∇
·
ξ
⊥
,
=
=
u
=
∂
ξ
1
c
u
∂t
,
E
⊥
=
−
×
B
0
,
E
=
E
z
=0
.
(4.26)
Here
b
⊥
,
E
⊥
and
b
,E
are magnetic and electric wave components perpen-
dicular and parallel to the ambient magnetic field
B
0
.
Alfven Waves
A wave with zero perturbations of density
ρ
1
and field-aligned displacement
ξ
can be excited in plasmas. As a consequence, the wave field-aligned magnetic
component
b
=
−
B
0
∇
·
ξ
⊥
also vanishes. In this case the wave should carry
with it a non-zero vortex
Ω
=[
∇×
u
]
and a non-zero longitudinal component of current density
c
4
π
[
j
=
∇×
b
]
,
where
=
[
.
B
0
B
0
∇×
∇
×
·
[
b
]
b
]
This wave mode is called the Alfven wave [1]. Equations for the Alfven waves
can be found from (4.24)-(4.25). Transverse displacement
ξ
in an Alfven
⊥
wave is found from
=
∂
2
ξ
⊥
∂
2
ξ
⊥
∂t
2
1
c
2
A
L
ξ
∂z
2
−
=0
.
(4.27)
⊥
In addition, since
ρ
1
= 0, then it follows from (4.26) that
ξ
must be solenoidal
⊥
∇
·
ξ
⊥
=0
.
(4.28)
For an individual field-line, (4.27) coincides with the elastic string equa-
tion. According to (4.27), transverse displacement in an Alfven wave propa-
gating in the positive
z
direction is
ξ
(
x, y, z, t
)=
ξ
+
(
x, y, ζ
)
,
ζ
=
z
−
c
A
t,
(4.29)
⊥
where
ξ
+
(
x, y, ζ
)ateachfixed
ζ
is an arbitrary solenoidal 2D vector field
orthogonal to
B
0
.From
∇
·
ξ
⊥
= 0 it follows that
ξ
⊥
canbeexpressedin
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