A unified theory is developed which describes nonlinear evolution of s
urface gravity waves propagating over an uneven bottom in the case of
two-dimensional incompressible and inviscid fluid of arbitrary depth.
Under the assumptions that the bottom of the fluid has a slowly varyin
g profile and the wave steepness is small, a system of approximate non
linear evolution equations (NEEs) for the surface elevation and the ho
rizontal component of surface velocity is derived on the basis of a sy
stematic perturbation method with respect to the steepness parameter.
A single NEE for the surface elevation is also presented. These equati
ons are expressed in terms of original coordinate variables and theref
ore they have a direct relevance to physical systems. Since the formal
ism does not rely on the often used assumptions of shallow water and l
ong waves, the NEEs obtained are uniformly valid from shallow water to
deep water and have wide applications in various wave phenomena of ph
ysical and engineering importance, The shallow- and deep-water limits
of the equations are discussed and the results are compared with exist
ing theories. It is found that our theory includes as specific cases a
lmost all approximate theories known at present.