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) T 1 (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.
Purchased from American Mathematical Society for the exclusive use of nofirst nolast (email unknown) Copyright 2014 American Mathematical Society. Duplication prohibited. Please report unauthorized use to cust-serv@ams.org. Thank You! Your purchase supports the AMS' mission, programs, and services for the mathematical community.
