Research Article A Homotopy-Analysis Approach for Nonlinear Wave-Like Equations with Variable Coefficients Afgan Aslanov Mathematics and Computing Department, Beykent University, 34396 Istanbul, Turkey Correspondence should be addressed to Afgan Aslanov; afganaslanov@beykent.edu.tr Received 20 February 2015; Accepted 23 April 2015 Academic Editor: R. Naz Copyright © 2015 Afgan Aslanov. Tis is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. We are interested in the approximate analytical solutions of the wave-like nonlinear equations with variable coefcients. We use a wave operator, which provides a convenient way of controlling all initial and boundary conditions. Te proposed choice of the auxiliary operator helps to fnd the approximate series solution without any discretization, linearization, or restrictive assumptions. Several examples are given to verify the reliability and efciency of the method. 1. Introduction We consider the equation  −(,)  =(, , ,  )+(,), >0,>0 (1) with initial conditions (,0)=(), (,0)=() (2) and boundary condition (0,)=ℎ(), (3) where , , , , , and are known functions. Note that the proposed method can be applied for equations like (,)  −  =(, , ,  )+(,), (4) with the same type of initial-boundary conditions. Problems like (1)(3) model many problems in classical and quantum mechanics, solitons, and matter physics [1, 2]. If is a function of only and (,)= const we obtain Klein- Gordon or sine-Gordon type equations. Tese models can describe some nonlinear phenomena; for example, wave-like equation can describe earthquake stresses [3], coupling cur- rents in a fat multistrand two-layer superconducting cable [4], and nonhomogeneous elastic waves in soils [5]. Typical examples of the wave-like equations with variable coef- cients are Euler-Tricomi equation [6] or Chaplygin equa- tion [7] given by  −  =0,  −()  =0, (5) which are useful in the study of transonic fow, where = (,) is the stream function of a plane-parallel steady-state gas fow, () is positive at subsonic and negative at supersonic speed, and is the angle of inclination of the velocity vector. Some Chaplygin type of equation of the special form  + 2 1− 2 / 2  + =0, (6) where =() is the speed of sound, has also applications in the study of transonic fow [8]. Note that we use the term wave-like equation to describe the partial diferential equations with the terms  and  ; that is, the term “wave-like” may not correspond to the real physical waves, in general. Recently, there has been a growing interest for obtaining the explicit solutions to wave-like and heat-like models by Hindawi Publishing Corporation Abstract and Applied Analysis Volume 2015, Article ID 628310, 7 pages http://dx.doi.org/10.1155/2015/628310