Accurate measurements of the kinematics under wave crests in uni-direc
tional, one and two component wave groups in a flume have produced the
following conclusions: The wave group length affects the internal wav
e kinematics. Waves in shorter wave groups can produce higher wave kin
ematics above still water level than similar waves in longer groups. R
egular waves can be accurately modelled using a higher order regular w
ave Fourier theory provided Stokes' second definition of wave celerity
is used. Steep, near-breaking two-component waves can be modelled acc
urately using a derivative of linear theory, here superposition stretc
hing. Measurements should be made above mean water level, if experimen
tal results are to have much credence.