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An analysis of the large‐scale features of the upper troposphere and the stratosphere in a global, three‐dimensional, general circulation model

The formulation of a 13–Ievel general circulation model of the troposphere and stratosphere is described and an account given of the climatology produced from an annual integration. Emphasis is placed on the interhemispheric differences in the stratosphere and the seasonal variability exhibited by its circulation. Overall, a realistic simulation of various features of the large‐scale tropospheric and stratospheric flow patterns was achieved, although a number of shortcomings are noted.