Huang, R-X., and K. Bryan, 1987: A multilayer model of the thermohaline
and wind-driven ocean circulation. Journal of Physical Oceanography,
17(11), 1909-1924.
Abstract: A hybrid, multilayer model for the oceanic general
circulation is formulated and tested. The model includes a mixed layer
at the surface which is specified by Eulerian coordinates, and three moving
layers below which are specified by quasi-Lagrangian, isopycnal coordinates.
Initial tests have been carried out with a 22 x 22 horizontal grid mesh
covering a subtropical-subpolar basin (6000 x 6000 km2).
The numerical results demonstrate a strong interaction between the wind-driven
and the thermally driven circulations, including outcropping of the lower
isopycnal layers, a Gulf Stream-like interior boundary current, and convection
which produces mode water and abyssal water. The model provides insight
into the potential vorticity balance and its relation to both the wind-driven
and thermohaline components of the circulation which has not been previously
available from Eulerian numerical models or analytical models based on
the assumption of an ideal fluid thermocline.