IIRC (which I might not — twas a while ago), in our MIROC ensemble (
slab ocean GCM), members with high eqm climate sensitivity also had high control temperature.
Not exact matches
The mean and median of the equilibrium land -
ocean warming contrast (using a
slab ocean) in the
GCMs considered is ~ 1.3 (with a spread of about 1.2 - 1.5).
Left column is the name of ensembles, and in the second left column, «AOGCM» denotes atmosphere —
ocean coupled
GCM, and «ASGCM» denotes atmosphere -
slab ocean coupled
GCM.
«CMIP3 - AO» denotes twentieth century experiment by atmosphere —
ocean coupled general circulation model (
GCM), and «CMIP3 - AS» denotes control experiment by atmosphere -
slab ocean coupled
GCM.
The response of the ITCZ to extratropical thermal forcing: idealized
slab -
ocean experiments with a
GCM.