This paper describes the global ocean component of the NCAR Climate Sy
stem Model. New parameterizations of the effects of mesoscale eddies a
nd of the upper-ocean boundary layer are included. Numerical improveme
nts include a third-order upwind advection scheme and elimination of t
he artificial North Pole island in the original MOM 1.1 code. Updated
forcing fields are used to drive the ocean-alone solution, which is in
tegrated long enough so that it is in equilibrium. The ocean transport
s and potential temperature and salinity distributions are compared wi
th observations. The solution sensitivity to the freshwater forcing di
stribution is highlighted, and the sensitivity to resolution is also b
riefly discussed.