1.1. ENERGY BALANCE MODELS OF CLIMATE DYNAMICS 5
0 2 · 105 3 · 105 4 · 105 105
time
T ε(t)
T3(t)
T1(t)
Figure 1.6. A typical solution trajectory of equation (1.2) for the
small noise amplitude.
0 2 · 105 3 · 105 4 · 105 105
time
T ε(t)
T3(t)
T1(t)
Figure 1.7. A typical solution trajectory of equation (1.2) for
the large noise amplitude.
0 2
· 105
3 ·
105
4 ·
105 105
time
T ε(t)
T
3
(t)
T1(t)
Figure 1.8. A typical solution trajectory of equation (1.2), the
noise amplitude well tuned.
curves are well tuned with the periodic input. A typical well tuned curve is shown
in Figure 1.8.
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