Existence of weak solutions to the 3-D semi-geostrophic equations with rigi
d boundaries was proved by Benamou and Brenier [3], using Monge transport t
heory. This paper extends the results to a flee surface boundary condition,
which is more physically appropriate. This extension is at present for the
2-D shallow water case only. In addition, we establish stronger time regul
arity than was possible in [3].