Geoscience Reference
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1+ α (0)
,
+ γ (0)
0
O 2 = α (0)
0
( b 1 cos 2 Ωt
a 1 sin 2 Ωt )+
···
(13.13)
0
2
+ γ (0 0 1+
[N e ]= α (0)
0
α (0)
0
d 1 cos 2 Ωt
1
2
b 1 + γ (0)
0
α (0 0 a 1 + γ (0 0 c 1 sin 2 Ωt +
,
···
(13.14)
where α (0)
0
and γ (0)
0
are found from the averaged equations (13.6), (13.7):
α (0)
0
+ γ (0 0 =0 ,
(0)
0
a 0 α (0)
I 1
0
α (0)
0
+ γ (0 0 =0 .
I 2 + (0)
c 0 α (0)
(13.15)
0
0
Suppose now that the pump wave amplitude is modulated by the harmonic
oscillations sin Ωt. Then T e fluctuations are proportional to sin 2 Ωt . The total
electron temperature T e is given by T e = T 0 + T 1 sin 2 Ωt. We find α (0)
and
0
γ (0)
0
from (13.15), substitute them into (13.13) and (13.14) and obtain the
time dependencies of O 2 and [N e ] . Figure 13.3 (curves 7 and 8 for periods
τ T =10sand τ T = 100 s, respectively) shows the dependence of the depth of
modulation p m = δN e / [ N e (max) + N e (min)] of N e on T 1 /T 0 .
10 0
5
τ T = 100 s
6
2
8
4
1
10 −1
τ T = 10 s
3
7
10 −2
0
2
4
6
8
10
T 1 /T 0
Fig. 13.3. Relative amplitude of oscillations of the electron concentration p m =
δN e / [ N e (max) + N e (min)] = [ N e (max) − N e (min)] / [ N e (max) + N e (min)] as a func-
tion of the temperature modulation T 1 /T 0 for τ T =10and τ T = 100 s. Curves 1,2
correspond to 10/100s minimum solar activity. Curves 3,4 are for maximum activity.
Curves 6 and 5 represent the dependency p m ( T 1 /T 0 ) for the long time modulation
( τ T chem 1) for the minimum and maximum solar activity, respectively. The
dashed lines labeled 7 and 8 respect to the fast modulation ( τ T chem 1) are the
integrand of (13.13)-(13.14) for τ T = 10 and 100 s correspondingly
 
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