“…We consider a general formulation on steady or quasi-steady state hydrodynamically fully developed and thermally developing convection, that governs the temperature field T(x, z), dependent on the position x on the transversal plane and on the longitudinal coordinate z, defined in the transversal region V with boundary surface S. The formulation includes the convection term, the diffusion operator, a linear dissipation term, and an independent source term [13], as shown in problem (1) below. The coefficients w(x), k(x), and d(x), are responsible for the information related to the velocity field, geometry and eventually even heterogeneity of the medium.…”