The study of wave generation on elastic coatings in inconipressible fluid flows is of interest for using these coatings to decrease the drag and suppress acoustic noise and vibrations [1,2]. Up to now, the main attention was focused on the linear theory of instability arising upon interaction of elastic coatings of various types with a laminar flow (see the review of literature in [3]). The problem of excitation of finit~amplitude waves was also solved for a lamfimr flow regime [4,5].Generation of wave, s on elastic coatings in a turbulent boundary layer (TBL) was experimentally studied in some papers [1,6]. Two 1)~usie regimes of generation of hydroeb~stic waves were ~bund: traveling-wave flutter (T~VF) and wave divergence. Reutov and Rybushkina [7] used an algebraic model of vortex viscosity to study linear hydroelastic instability in the TBL, and equations for two-(timensional wave perturbations in the boundary layer were written in curvilinear coordinates. The calculated vahles of the critical velocity of TWF and wave-divergence origimttion are in good agreement with the experimental data of [1,6]. Reutov [8] proposed a immerical model, which allows one to calculate the nonlinear response of the TBL to a wavy flexure of the underlying surface. As in [9], where the interaction of waves on water with an atmospheric TBL was examined, Reutov [8] used a quasi-linear approximation, where the basic nonlinear effects are related to deformation of the profile of the mean (over the waviness period) flow.In tile present paper, which should be considered as a continuation of [7,8], we study the nonlinear stage of evolution of hydroelastic instability in the TBL on a single-layer coating. The main small parameter of the problem is tile slope of the wavy surface ka << 1 (k and a are the wavenumber and the amplitude of surface flexure). Another limitation of the proposed theory is the fact that the surface flexure has the form of a two-dinmnsional quasi-monochromatic wave.In the above-cited experiments [1, 6]~ the flow velocity could exceed the critical value by several times. Waves with large slopes of the surNce were observed. The approach proposed in the i)resent paper allows one to consider tile region of small and moderately small supercritical vahles at which rather weak waves are generated. V~e note that generation of divergent waves with huge slopes of the sm'face were immerically simulated by Lucey and Carpenter [10]. However, the potential-flow approximation wa,s used in the latter Institute of Applied Physics, Russian A(:ademy of Sciences, Nizhnii Novgorod 603600.