Bryson (1978) has suggested that weather variations of up to about 10 days are primarily hydrodynamic in character, while longer term changes are primarily thermodynamic and depend on the boundary conditions. The boundary conditions include sea surface temperatures, the distribution of snow and ice, surface albedo, atmospheric composition, and variations in solar radiation. These boundary conditions mostly influence climate by changing the distribution of energy inputs and exchanges. Feedback mechanisms are particularly important in the amplification of small changes in the boundary conditions. Such mechanisms act as internal controls of the climatic system, and display a coupling or mutual compensation among two or more elements of the climatic system. The best known positive feedback mechanism is the snow-albedo-temperature system, in which an increase of snow cover increases the surface albedo and thereby lowers the surface temperature. This decrease in surface temperature leads, all else being equal, to further increases in the extent of snow cover and still lower surface temperatures. Obviously, any positive feedback must be checked at some level by the intervention of other internal adjustment processes, or the climate would exhibit a runaway behaviour.Considerations of feedback mechanisms lead to the definition of climate as the equilibrium state reached by the elements of the atmosphere, hydrosphere, and cryosphere under a set of given and fixed input conditions. Some of the recent research on each of the important boundary conditions is reviewed in this paper. Indirectly, the sun drives all the meteorological at RMIT UNIVERSITY on August 11, 2015 ppg.sagepub.com Downloaded from