Coastal Trapped Waves Propagation Along The Southwestern Atlantic Continental Shelf

This study investigates the propagation of coastal trapped waves (CTWs) along the Brazilian continental shelf between 34 degrees S and 11 degrees S using in situ data combined with the outputs from a high-resolution ocean simulation with HYCOM. The CTWs generation area covers a wide region ranging from the Patagonian shelf to the southern Brazilian shelf. The spectral analysis of coastal sea level series between 54 degrees S and 10.5 degrees S shows three bands of high energy associated with periods from 5 to 12 days, 15-22 days, and 25-40 days. The energy of the CTWs decreases along their propagation for all frequency bands, showing a drastic reduction north of 22 degrees S, due to abrupt variations in the width and depth of the continental shelf between Tubara similar to o Bight and Abrolhos Bank. Their phase speed propagation varies along the coast, being faster (>25 m/s) in the southernmost region (between 42 degrees S and 41 degrees S), reaching -11 m/s north of 41 degrees S, and reducing to -3 m/s further north (equatorward of 24 degrees S). The free Continental Shelf Wave theory supports the notion that the intense deceleration north of 24 degrees S can be explained by the narrowing of the continental shelf. The stratification parameter indicates that the Brazilian continental shelf has a barotropic response to wind-generated disturbances.