“…In the studies involving open cavity natural convection, two basic boundary wall conditions are observed: (a) all the walls of the open cavity were heat transfer surfaces at constant temperature [1,2,4,6,8,9,12,18,19,21,22,25,26,[30][31][32], henceforth referred to as isothermal wall boundary condition and (b) only one wall (wall opposite to the aperture) was at constant temperature and the remaining walls were kept adiabatic, henceforth referred to as constant temperature back wall boundary condition [3,5,10,11,13,20,23,24,33]. Other wall boundary conditions such as one wall having constant heat flux and other walls being adiabatic [14][15][16] and nonisothermal wall temperatures [7,[27][28][29] were also studied.…”