"The flow is turbulent, the velocity v (x, y, z, t) of the wind can be considered as the superposition of the mean velocity v (x, y, z) which changes only slowly with time, and a fluctuation rate v ¢ (x, y, z, t) can be treated as a dependent random process the space and time.

Given the time scales considered (hours, minutes) in the studies of sea keeping structures, the description of wind can be made ​​by assuming that the mean component is independent of time and the fluctuating component is part of a stationary, ergodic and Gaussian process."

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