Close physical analysis of free convection and the associated vertical buoyancy and density forces shows that they do not exist in a natural continental subsurface environment. All density and buoyancy derivedforces need to be included by modifying the length of the pressure potential forces of fresh...
In this paper, we derive a quasilinear second-order partial differential equation which has to be satisfied by surfaces around which 3D free convection boundary layer flows can be two-dimensionalized. It is obtained from the boundary layer equations which are expressed in a system of curvilinear ...