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N 0 (3 10 25 cm 23 )
T 5 2501 sec
T
5
2501 sec
0.0
0.5
1.0
1.5
2.0
2.5
5.0
550
4.0
3.0
2.0
1.0
0.0
21.0
22.0
2
500
450
400
3.0
2
350
4.0
25.0
2
300
240
2
120
0
(km)
120
240
2
240
2
120
0
120
240
East
West
East
(km)
West
(a)
N 0 (3 10 25 cm 23 )
N 0 (3 10 25 cm 23 )
T 5 2106 sec
T 5 2250 sec
550 0.0
0.5
1.0
1.5
2.0
2.5
550 0.0
0.5
1.0
1.5
2.0
2.5
500
500
450
450
400
400
350
350
No resonance
No resonance
300
300
2
200
2
100
0
100
200
2
200
2
100
0
100
200
East
(km)
West
East
(km)
West
10 25 cm 23 )
10 25 cm 23 )
T
5
1750 sec
N 0 (
3
T
5
1920 sec
N 0 (
3
0.0
0.5
1.0
1.5
2.0
2.5
0.0
0.5
1.0
1.5
2.0
2.5
550
550
500
500
450
450
400
400
350
350
At resonance
At resonance
300
300
2200
2100
0
100
200
2200
2100
0
100
200
East
(km)
West
East
(km)
West
(b)
Figure 4.17 (a) Evolution of gravity wave seeking with no amplification by the Rayleigh-
Taylor instability. (b) Evolution with gravitation included, both at resonance and without
resonance. [After Huang and Kelley (1986). Reproduced with permission of the American
Geophysical Union.]
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