The boundary layer convection with uniform heat flux from the side walls of an inclined rectangular enclosure

This paper is the analysis of buoyancy driven convection in an inclined fluid filled rectangular enclosure. The existence of constant heat flux heating and cooling through the walls of the vertical side. It is demonstrate analytically that of the boundary layer thickness must be independent of altitude in the boundary layer regime, that the core must be linearly stratified and motionless, and that the temperature of the vertical inclined walls must vary continuously as the core temperature with the same gradient.