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CLIMATE MODELS ARE quantitative representations of the earth, its atmosphere, and the ways in which they interact to influence the climate. Models range from the comparatively simple to the extremely complex and their range, complexity, and predictive power have increased significantly in the 21st century as computational power has increased. The ability of scientists to create sophisticated climate models is of several magnitudes of order beyond what was possible even a few years ago.

Scientists use mathematical formulae, combined with the modeling ability of computers and available data sources, to create an understanding of how climate and weather effects work in different parts of the atmosphere. The purpose of the models is not just to understand atmospheric interactions, however, but to predict how they will work in the future. Predicting the weather will be of great benefit in helping people prepare for adverse phenomena such as hurricanes and typhoons, as well as the longer-term effects of drought or floods.

Further, as evidence has begun to accumulate that increased release of carbon dioxide and other gases is having a significant effect on the warming of the atmosphere, climate models have acquired the additional role of predicting the future of the world's climate and the effect of constant warming of the atmosphere.

This has led to some controversy because there are powerful economic and political incentives for some to try to demonstrate that atmospheric warming, and hence, global climate change, is not a long-term, persistent phenomenon or, if it is, that it is the result of human actions. Climate scientists have found themselves, their motives, and their methodologies questioned, much more fiercely than before and not every scientist has been comfortable with this development.

Academic discourse and the scientific method require knowledge to be accumulated in a systematic method subject to peer review, which means that most scientists are, quite properly, hesitant about giving simple, unequivocal answers to questions that require ‘yes’ or ‘no’ answers. The entire academic process is not transparent to outsiders and it is difficult to refute criticism.

The Scientific Basis

The fundamental climate change equation concerns the exchange of heat in the atmosphere. Heat is transmitted to the atmosphere from radiation from the Sun. Some of the heat energy is absorbed and some reflected. The amount of energy reflected depends on the albedo of the surface and can be affected by variables such as color, elevation, and shape. If more energy is retained than reflected, then the atmosphere will increase in temperature, but temperatures will decrease if the opposite is true. This equation is affected by the composition of the atmosphere, among many other factors. While the equation appears navigable, in fact the complexity of the atmosphere is such that it is extremely difficult to write accurately.

Scientists in the 19th century attempted to create the equation using the mathematical and analytical tools available. At that time, the number of atmospheric observations and the extent of their coverage were very limited. As observations improved in quality and quantity, the ability to model the equation improved. Scientists realized that the wind system was not consistent acround the world and, consequently, what happened in one part of the world was different from another part of the world, even with similar initial conditions. Consequently, it became a logical step to divide the surface of the world into smaller subsections on a grid basis and attempt to solve the equations and, hence, predict the weather, for each grid square.

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