A submerged hydrofoil generated large steady breaking waves of 0.3 m and 0.
4 m height in a circulating water channel. We measured water fraction in th
e breakers with conductivity probes. We observed the radar cross-section of
the breakers at X-band with a pulsed step-frequency instrumentation radar
with high spatial resolution in the downstream direction. The normalized ra
dar cross-section increases with increasing elevation angle of observation
for both vertical and horizontal polarization. This variation is consistent
with a simple interpretation of the breaking wave as a diffuse (Lambertian
) surface. However, the observed sizes and shapes of fluid elements in the
breakers clearly show that construction of a theory for electromagnetic sca
ttering from first principles will be challenging. We also obtained the vel
ocity spectrum of the scattering features within the breakers. This spectru
m indicates that slower moving small liquid elements rather than the faster
moving large disturbances are responsible for most of the electromagnetic
scattering.