. The 2nd-order bistatic high-frequency radar cross section of ocean surface is derived for the case of a fixed receiver and a floating transmitter. The 2nd-order radar cross section contains both the hydrodynamic contribution and the electromagnetic contribution. The 2nd-order hydrodynamic contribution is obtained based on the 1st-order bistatic model with antenna motion. The derivation of the 2nd-order electromagnetic contribution begins with a general expression for the bistatically received 2nd-order electric field for the case of a floating antenna. A new bistatic electromagnetic coupling coefficient, which, unlike some earlier versions, produces no nonphysical singularities in the radar cross section, is derived. The new bistatic radar cross section model is verified by comparing it with that of a monostatic swaying antenna case and that of the bistatic case without antenna motion. The effect of platform motion on simulated Doppler spectra is considered for a variety of sea states and operating frequencies. The motion-induced 2nd-order peaks appearing in the spectrum are seen to have significantly less energy than those in the 1st-order case.
Read full abstract