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The statistical distributions for the elevation,velocity and acceleration of the surface of wind waves
Authors:Tadao Honda  Hisashi Mitsuyasu
Institution:(1) Research Institute for Applied Mechanics, Kyushu University, Hakozaki, Higashi-ku, 812 Fukuoka, Japan
Abstract:Water surface elevationseegr(t), vertical surface velocities 
$$\dot \eta (t)$$
and vertical surface acceleration 
$$\dot \eta (t)$$
of wind-generated waves have been measured in a laboratory wind wave channel by using resistance-type wave gauges combined with an electronic differentiation circuits. Probability distributions of the values ofeegr(t), 
$$\dot \eta (t)$$
, and 
$$\ddot \eta (t)$$
have been determined from the wave records.In an initial stage of wave generation,i.e., when wind waves are generated at short fetches and low wind speeds, the observed distributions foreegr(t), 
$$\dot \eta (t)$$
and 
$$\ddot \eta (t)$$
are appreciately good fit to the distributions given by successive sum of a Gram-Charlier series, which has been derived following the formulation ofLonguet-Higgins (1963), by taking the weakly nonlinear effect into account.However, when wind waves develop with increasing wind speeds and fetches, the observed distributions deviate gradually from the Gram-Charlier series. Particularly, the deviations are remarkable for the distribution of 
$$\ddot \eta (t)$$
.When the wind speed increases, the observed distributions ofeegr(t), 
$$\dot \eta (t)$$
and 
$$\ddot \eta (t)$$
show the following characteristics: (i) the skewnesses of the distributions ofeegr(t) and 
$$\dot \eta (t)$$
decrease slightly, (ii) the skewness of 
$$\ddot \eta (t)$$
changes, at some wind speed, from positive small values to relatively large negative values, (iii) the kurtosis of the distribution ofeegr(t) decreases slightly but that of 
$$\dot \eta (t)$$
increases slightly and these characteristics seem to depend not so much on fetches, (iv) the kurtosis of the distribution of 
$$\ddot \eta (t)$$
increases rapidly.
Keywords:
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