“…(1) (2) (3) (4) The velocity vector q and its magnitude q are defined in terms of the cartesian velocity components, dt where + V -(pqS) = 0 (5) S = In (^ ^ } (6) which shows that the entropy 5 should be constant throughout the flow if it is constant at the upstream boundary. In practice, however, the discrete forms of equations (1,2,3,4) must be stabilized with dissipative terms, which either appear naturally as truncation errors or are added explicitly, depending on the discretization scheme used.…”