The idealized GCMs described above are flexible and general enough that it is relatively straightforward to convert them into GCMs for other planets, for example, with
different planetary rotation rates and radii and with different thermodynamic properties of the atmosphere, condensable species, and surface.
vukcevic, The only thing I would know of changing currents is by the
different balance this planet has with the
different mass differences to water distances with
rotation that would generate the
planetary wobble.