Abstract

In this study, we embark on analytical determination of oceanic climate model in consideration of damped oscillations. The formulation contains two small but independent parameters which are used in asymptotic expansions of variables, and because of non-uniformity in asymptotic expansions, we used Lindstendt-Poincare perturbation technique to obtain the approximate solution of the model.

Keywords: Perturbation technique, Lindsted-Poincare, oceanicclimate change, Pacific Ocean, thermocline,damped oscillations.