The effect of wind irregularities on fluctuations of the spectral comp
onents of ambient sea noise is analyzed. Experimental examples are use
d to demonstrate that the parameters of the noise envelope depend on t
he relation between the spatial scales of wind disturbances and the si
ze of the hydrophonically covered region on the sea surface. A conveni
ent noise-field modeling concept of a radial function of hydrophone se
nsitivity to distributed surface dipole noise sources is introduced. T
his hydrophone surface sensitivity function (SSF) depends on the sound
velocity profile, hydrophone submersion depth, frequency-dependent ab
sorption in the medium, bottom reflectivity, and scattering of sound i
n the bulk and from the boundaries of the waveguide. The characteristi
cs of noise fluctuations are determined by convolving the SSF with a m
oving mosaic of wind gusts. It is demonstrated that the SSF integrates
small-scale wind gusts, and the dimension of the averaged surface flu
ctuations of wind speed are greater the deeper the hydrophone. Experim
ental results proved the adequacy of the noise-field fluctuation model
built around the SSF. It is demonstrated that the wind speed, locally
measured above the point of sound measurement, need not always define
the level of noise and parameters of its fluctuations.