Geoscience Reference
In-Depth Information
3. Slow magnetosonic waves: ion sound which at β<< 1 almost does not
disturb the magnetic field. The plasma is seemingly 1D-density perturba-
tions caused by longitudinal plasma displacements are transmitted along
the magnetic field at sound velocity c s .
If the parameter β is finite, magnetosonic waves cannot be precisely sepa-
rated into the FMS and ion sound. Coupling equations (4.33) and (4.34) must
be investigated. Let us apply Fourier transform decomposing the signal into
its harmonic components
ξ exp(
iωt + i kr )
d b exp(
iωt + i kr ) .
Equations (4.27), (4.28) for Alfven waves and (4.33), (4.34) for FMS-waves
reduce to:
Alfven waves
k 2
ξ =0 ,
ω 2
c 2 A
( k
·
ξ )=0 .
(4.37)
Magnetosonic waves
βξ + ω 2
b B 0
ik k 2
k 2
βk 2
c 2 A
=0 ,
(4.38a)
ω 2
c s
ξ
b B 0
k 2
ik
=0 ,
(4.38b)
where k and k are the values of the perpendicular and parallel to the mag-
netic field B 0 components of the wave vector k .
A uniform linear system of algebraic equations has a non-trivial solution
only in the case of the zero determinant of this system. Since the deter-
minant
( ω, k ) is a function of ω and k , this condition results in a
functional relation between frequency ω and wave vector k , designated as the
dispersion equations which are given by
Alfven waves
ω 2
k 2
c 2 A =0 .
(4.39)
Magnetosonic waves
c 2 A + c s k 2
ω 4
ω 2 + c 2 A c s k 2
k 2 =0 .
(4.40)
A presentation of magnetohydrodynamic waves in homogeneous plasma
can be given in the form of an angle dependency of phase velocity V ph = ω/k
on angle θ between k and B 0 . Then substitution k = k cos θ into (4.39) and
(4.40) leads to
V ph = V A = c 2 A cos 2 θ
for the Alfven waves and
± c 2 A + c s V 2
V 4
+ c 2 A c s cos 2 θ =0
±
 
Search WWH ::




Custom Search