The sensitivity of a coupled ocean-atmosphere general circulation mode
l to parameterizations of selected physical processes is studied. The
parameterizations include those of longwave radiation and surface turb
ulent fluxes in the atmospheric model, and those of vertical turbulent
mixing and penetration of solar radiation in the ocean model. It is s
hown that the performance of the coupled model is highly sensitive to
the parameterization of longwave radiation. This sensitivity is not so
lely due to the difference in surface radiative flux but involves inte
ractions among radiation, convection, and large-scale dynamics of the
atmosphere and ocean. It is concluded that differences in parameteriza
tions can have large impacts on the performance of the coupled model,
and these impacts can be very different from what may be expected from
uncoupled model simulations.