статья в журнале

En

Remote Sensing
eSSN:2072-4292

2021

Grodsky, S.A.¹

Chapron, B.²

10.3390/rs13101929

The effective normalized radar cross section (NRCS) of breaking waves, sigma wb, is empirically derived based on joint synchronized Ka-band radar and video records of the sea surface from a research tower. The sigma wb is a key parameter that, along with the breaker footprint fraction, Q, defines the contribution of non-polarized backscattering, NP =sigma wbQ, to the total sea surface NRCS. Combined with the right representation of the regular Bragg and specular backscattering components, the NP component is fundamental to model and interpret sea surface radar measurements. As the first step, the difference between NRCS values for breaking and non-breaking conditions is scaled with the optically-observed Q and compared with the geometric optics model of breaker backscattering. Optically-derived Q might not be optimal to represent the effect of breaking waves on the radar measurements. Alternatively, we rely on the breaking crest length that is firmly detected by the video technique and the empirically estimated breaker decay (inverse wavelength) scale in the direction of breaking wave propagation. A simplified model of breaker NRCS is then proposed using the geometric optics approach. This semi-analytical model parameterizes the along-wave breaker decay from reported breaker roughness spectra, obtained in laboratory experiments with mechanically-generated breakers. These proposed empirical breaker NRCS estimates agree satisfactorily with observations.

ackscatter, reaker, reaking wave, ield measurements, a-band, ambda-distribution, malized radar cross-section, cean, Rada

2021-07-20 14:01:50