“…One of the effective mechanisms that control convective instability is that of maintaining a nonlinear temperature gradient. Recently, considering various convective flow models in porous medium [5][6][7], fluid layer [8][9][10] the phenomenon of heat or mass transfer investigated, where the concept of regulating either heat or mass transfer is missing. The temperature gradient can be achieved by time-dependent heating or cooling at the boundaries, the related problems have been investigated by Nield [11], Chhuon and Caltagirone [12], Rudraiah et al [13], Rudraiah and Malashetty [14], Caltagirone [15], Bhatia and Bhadauria [16,17], Bhadauria [18][19][20][21][22][23][24], Bhadauria and Suthar [25], Bhadauria and Srivastava [26], Bhadauria et al [27], Bhadauria and Kiran [28,29] and Kiran and Bhadauria [30].…”