It is a highly complex system consisting of five main components: the atmosphere, the hydrosphere, the cryosphere, the earth's surface, and the biosphere, and the interrelationships between them. The last four subsystems represent the active surface. Solar energy that enters the interaction between the atmosphere and the active surface is the driving force behind meteorological and climate changes. The existence of the Earth's climate system can be dated back to the formation of the atmosphere, roughly 4.5 billion years. Subsequently, other components of the system were created, which significantly interact with each other and influence each other. Each of these components represents a complex thermodynamic system in which a large number of physical and chemical processes take place. There is a constant exchange of mass and energy between the individual components of the climate system. The climate system is therefore a very complex non-linear system.
A typical feature of the climate system is that it is constantly changing and developing, and it is also so complex that current science cannot fully accurately describe and predict its further development.