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Fig. 11


Zonally and temporally averaged (over a period of ≈30 yr) stream function for two models with either a relatively “strong” (Gleft – log (τ220) = 15) or very weak (Hright – log (τ220) = 20) isothermal relaxation (cooling) in the deep atmosphere (P > 10 bar). Clockwise circulations on the meridional plane are shown in red and anticlockwise circulations are shown in blue. Additionally, the zonally and temporally averaged zonal wind is plotted in black (solid = eastward, dashed = westward).

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