Images of a field of breaking waves over the ocean obtained using a li
ne-scanner on an aircraft are analyzed for a possible fractal geometry
. The cumulative probability function of the intensity is shown to be
self-similar for sufficiently large intensities occupying about 10% of
an imaged area. This structure is invariant to successive averaging o
ver successively larger boxes. A box-counting technique was applied to
images of one representative flight. The estimated fractal dimension
decreases from about 2.25 for a 10% areal coverage to about 1.7 for 0.
1% coverage. It is concluded that the spatial distribution of the scat
tered light from foam and whitecaps is not monofractal, but is instead
multifractal.