| description abstract | stimation of second-order, near-surface wave kinematics is important for interpretation of ocean surface remote sensing and surface-following instruments, determining loading on offshore structures, and understanding of upper ocean transport processes. Unfortunately, conventional wave theories based on Stokes-type expansions do not consider fluid motions at levels above the unperturbed fluid level. The usual practice of extrapolating the fluid kinematics from the unperturbed free surface to higher points in the fluid is generally reasonable for narrow-band waves, but for broad-band ocean waves this results in dramatic (and non-physical) overestimation of surface velocities. Consequently, practical approximations for random waves are at best empirical and often only loosely constrained by physical principles. In the present work we formulate the governing equations for water waves in an incompressible and inviscid fluid, using a boundary-fitted coordinate system (i.e. ?sigma? or s-coordinates) to derive expressions for near-surface kinematics in nonlinear random waves from first principles. Comparison to a numerical model valid for highly nonlinear waves shows that the new results are 1) consistent with second-order stokes theory, 2) similar to extrapolation methods in narrow-band waves, and 3) greatly improve estimates of surface kinematics in random seas. | |
