MULTIPLE EQUILIBRIA IN 2-DIMENSIONAL THERMOHALINE CIRCULATION

As a model of the thermohaline circulation of the ocean we study the two-dimensional Boussinesq equations forced by prescribing the surface temperature and the surface salinity flux. We simplify the equations of motion using an expansion based on the small aspect ratio of the domain. The result is an amplitude equation governing the evolution of the depth averaged salinity field. This amplitude equation has multiple, linearly stable equilibria. The simplified dynamics has a Lyapunov functional and this variational structure permits a simple characterization of the relative stability of the alternative steady solutions. Even when the thermal and salinity surface forcing functions are symmetric about the equator there are asymmetric solutions, representing pole to pole circulations. These asymmetric solution are stable to small perturbations and are always found in con unction with symmetric solutions, also stable to small perturbations. Recent numerical solutions of the full two-dimensional equations have shown verv similar flow patterns.