It has been shown by Schlesinger and Mintz (1979) that the UCLA general
circulation model (GCM) is able to simulate the observed negative correlation
between the total amount of ozone in a vertical atmospheric column (the total ozone)
and the eastward-propagating synoptic disturbances in the troposphere, with the
total ozone...
The OSU global coupled atmosphere/ocean general circulation
model (A/O GCM) has been used to simulate the present (lxCO₂)
climate and to investigate a CO₂-induced (2xCO₂) climate change.
Previous analysis of the lxCO₂ simulation showed distinct errors in
the simulated sea surface temperature (SST) and sea ice which were
attributed primarily...