Modelling the global climate response to orbital forcing and atmospheric carbon dioxide changes

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Atmospheric Models, Carbon Dioxide, Insolation, Orbital Elements, Synoptic Meteorology, Atmospheric Chemistry, Climatology, Gas Density, Solar Terrestrial Interactions

Scientific paper

The operation of a global climate model which is forced simulataneously by changes in the distribution of solar insolation caused by orbital variations and by changes in atmospheric CO2 concentration, which are themselves forced by orbital parameters, is investigated. The model results show the potential importance of other components in the climate system and their associated response to changing orbital parameters.

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