IMAGING OF BIOGENIC AND ANTHROPOGENIC OCEAN SURFACE-FILMS BY THE MULTIFREQUENCY MULTIPOLARIZATION SIR-C/X-SAR/

Results from the analyses of several spaceborne imaging radar-C/X-band synthetic aperture radar (SIR-C/X-SAR) images are presented, which we re acquired during the two SIR-C/X-SAR missions in April and October 1 994 by the L-, C- and X-band multipolarization SAR aboard the space sh uttle Endeavour. The Images showing natural (biogenic) surface slicks as well as man-made (anthropogenic) mineral oil spills were analyzed w ith the aim to study whether or not active radar techniques can be app lied to discriminating between these two kinds of surface films. Contr olled slick experiments were carried out during both shuttle missions in the German Eight of the North Sea as well as in the northern part o f the Sea of Japan and the Kuroshio Stream region, where surface films of different viscoelastic properties were deployed within the swath o f the shuttle radars. The results show that the damping behavior of th e same substance is strongly dependent on wind speed. At high wind spe ed (8-12 m/s) the ratio of the radar backscatter from a slick-free and a slick-covered water surface (damping ratio) is smaller than at low to moderate wind speeds (4-7 m/s). At 12 m/s, only slight differences in the damping behavior of different substances were measured by SIR-C /X-SAR. Furthermore, several SAR scenes from various parts of the worl d's oceans showing radar signatures of biogenic as well as anthropogen ic surface films at low to moderate wind speeds are analyzed. The damp ing behavior of these different kinds of oceanic surface films varies particularly at L band where the biogenic surface films exhibit larger damping characteristics. Results of polarimetric studies from multipo larization SAR images showing various surface films are presented. It can be delineated from these results that Bragg scattering as well as specular reflection contribute to the backscattered radar signal at lo w incidence angles (up to 30 degrees). It is concluded that at low to moderate wind speeds, multifrequency radar techniques seem to be capab le of discriminating between the different surface films, whereas at h igh wind conditions a discrimination seems to be difficult.