In this study, the surface drift of an inextensible film due to a series of
progressive gravity waves is investigated both analytically and experiment
ally. A second approximation of the conformal mapping that transforms the p
rogressive sinusoidal surface to the horizontal axis is applied, thus allow
ing the analysis to formally accommodate a boundary layer thickness that is
much less than the wave height. By computing the stream function to the th
ird order that is an order higher than the past analysis, a pressure compon
ent in phase with the wave slope is revealed. The pressure force generated
is comparable to the bottom shear on the thin film induced by the moving fl
uid and thus cannot be ignored. Based on the combined forces on the surface
firm, a mean drift is estimated by assuming that the opposing force is due
to the viscous drag induced by the drift motion. The experimental results
show that the computed drift velocity based on the present study mostly und
erestimates the experimental observations, but it is in closer agreement th
an the classical Phillips' 7/4 estimate. (C) 1999 Elsevier Science Ltd. All
rights reserved.