Abstract
In this paper, we apply a new modification of the Adomian decomposition method for solving the problem of boundary layer convective heat transfer with viscous dissipation and low pressure gradient over a at plate. The technique is based on the standard Adomian decomposition method and the Chebyshev pseudospectral method. Comparisons are made between the pro-posed technique, the standard Adomian decomposition method, and the numerical solutions to demonstrate the applicability, validity, and high accuracy of the present approach. The results demonstrate that the new modification is more efficient and converges faster than the Adomian decomposition method. (C) 2018 National Laboratory for Aeronautics and Astronautics. Production and hosting by Elsevier B.V.