Geoscience Reference
In-Depth Information
1
1+
σ
i
/σ
e
.
j
e
=
j
But
m
e
m
i
σ
i
σ
e
∼
m
e
m
i
ν
e
ν
i
∼
1
,
where
m
i
being the average ion mass. Therefore
j
≈
j
e
.
This allows us to express
j
in terms of the magnetic pulsations components.
It follows from the Ampere's law that the vertical current density compo-
nent
j
z
is related with the magnetic wave components as
∂b
y
∂x
−
.
c
4
π
∂b
x
∂y
j
z
=
(12.24)
From an equation analogous to (12.23), but written for the total current, we
find
j
sin
I
=
j
z
+
σ
P
E
x
cot
I
+
σ
H
E
y
cos
I.
Taking into account that
j
e
≈
j
,
we rewrite (12.21)-(12.23)
j
xe
=
j
z
cot
I
+
σ
Pe
+
σ
P
cot
2
I
E
x
+
σ
He
+
σ
H
cot
2
I
E
y
,
σ
He
sin
I
E
x
+
σ
Pe
E
y
,
j
ye
=
−
j
ze
=
j
z
+
σ
Pi
E
x
cot
I
+
σ
Hi
E
y
cos
I.
(12.25)
For the electron velocity, we obtain from (12.25)
N
e
e
σ
Pe
+(
σ
Pe
+
σ
Pi
]cot
2
I
E
x
j
z
cot
I
N
e
e
1
v
xe
=
−
−
N
e
e
σ
He
+(
σ
He
+
σ
Hi
)cot
2
I
E
y
sin
I
1
+
1
N
e
e
σ
He
sin
I
E
x
−
1
N
e
e
σ
Pe
E
y
,
v
ye
=
j
z
N
e
e
−
1
N
e
e
σ
Pi
E
x
cot
I
1
N
e
e
σ
Hi
E
y
cos
I.
v
ze
=
−
−
(12.26)
Above the
E
-layer, the electron and ion Pedersen conductivities are small.
Neglecting collisions, we get
c
N
e
e
B
0
σ
He
=
−
σ
Hi
=
−
.
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