We will examine some aspects of the processes that determine the state of the climate The global Earth-system is modeled by non-linear systems. Each component
has a characteristic time scale associated with it. The entire Earth system is composed of the coupled interactions of these non-local, non-linear components. We will apply some analytic techniques specailly developed for the study of different time and dilation scales.
We will make an examination of critical greenhouse gas concentration trends and the data and theory of the Saturated Greenhouse Effect.
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