We subject
an aquaplanet GCM to a large array of different spatial patterns and magnitudes of ocean heat transport, and look at how variations in the transport affect aspects of the time - mean climate.
Included data files give fits to the CAM4
aquaplanet GCM simulations.
Levine, X. J., and T. Schneider, 2011: Response of the Hadley circulation to climate change in
an aquaplanet GCM coupled to a simple representation of ocean heat transport.
Not exact matches
The moist idealized
GCM has a spherical model surface that is entirely water covered (an «
aquaplanet»).