CORRELATION OF OCEANOGRAPHIC SIGNATURES APPEARING IN SYNTHETIC-APERTURE RADAR AND INTERFEROMETRIC SYNTHETIC-APERTURE RADAR IMAGERY WITH IN-SITU MEASUREMENTS

Synthetic aperture radar (SAR) imagery collected over the continental shelf near Cape Hatteras, N. C., is analyzed in conjunction with shipb oard hydrographic and current measurements. The SAR measurements were made over a 2-hour period on June 20, 1993, in both standard mapping m ode and interferometric synthetic aperture radar (INSAR) mode from a N ASA DC-8 aircraft as part of the High-Resolution Remote Sensing Experi ment. In situ currents were measured using a surface-towed acoustic Do ppler current profiler (ADCP). The measurements were made near the end of a period of Gulf Stream incursion onto the shelf as detected using a shore-based HF radar. Winds were southwesterly at 4-6 m s(-1). Long , curvilinear SAR signatures, resembling earlier SEASAT observations m ade in the same area, are shown to correspond to narrow, shallow front s separating water masses that increase in surface density with distan ce offshore. Across-front changes in surface current inferred from the INSAR data are consistent with 2-m-depth currents measured by the ADC P over scales of tens of meters. Thus frontal current gradients measur ed by INSAR reflect real changes in surface current and are not due to biases induced by changes in the surface-wave spectrum. This lends su pport to the detailed INSAR surface maps derived by Graber et al. [199 6]. An east-west salinity front having the largest observed surface de nsity and current gradient is corrugated on length scales up to the lo cal Rossby radius of deformation and translates southward between succ essive images. In data from the longer radar wavelengths the salinity front appears as a dark band downwind of a bright signature, and this is interpreted as a region where Bragg-scale waves regenerate followin g their dissipation in the frontal region. In addition to the fronts t he imagery shows closely spaced packets of southward propagating ocean internal waves occurring in the strongly stratified inshore water mas s. This case study further serves to emphasize the potential of SAR im agery for study of a wide range of shelf processes.