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
=[
∇×
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
 
Search WWH ::




Custom Search