In this paper we propose an iterative scheme for a nonlinear spherical geodynamo model and carry out convergence analysis of this scheme. Our model is a coupled system of fluid velocity u, total kinematic pressure P and magnetic field B. They are governed by the Navier-Stokes equations and the dynamo equations. Using the mathematical induction method and energy estimates, it is concluded that our iterative scheme converges in the L ∞ (0, T ; H 1 ) sense and in the L 2 (0, T ; H 2 ) sense.