An analysis of anomalous scattering behavior is performed on various corrug
ated surfaces relevant to oceanic scattering. In particular, it is shown th
at HH to VV ratios larger than 1 are produced as a result of polarization a
nomalies in the scattering returns. It is also shown that HH returns larger
than those predicted by first-order perturbation theory do occur. These ca
lculations thus provide the first evidence that some of the characteristics
associated with "sea spikes," found in backscatter measurements from the o
cean, can arise as a result of scattering from modulated wave trains. A qua
litative and quantitative correlation is observed between our analysis and
the water waves experiments of Lee et al. [1995].