USE OF TRANSIENT FEATURES TO IDENTIFY EASTWARD CURRENTS IN THE SOUTHERN-OCEAN

Sea surface temperatures and sea surface slopes, measured by the ERS-1 satellite, are used to investigate the propagation of mesoscale featu res in the Southern Ocean. The Antarctic Circumpolar Current (ACC) is clearly identifiable as a region of eastward propagation surrounded by mostly westward propagation. This confirms predictions based on resul ts from the Fine Resolution Antarctic Model, which suggest that the AC C is a region of flow which is supercritical with respect to the propa gation of baroclinic Rossby waves. This supercriticality allows the AC C to penetrate deep enough to interact with bottom topography and so m ay be an important part of the mechanism by which the current achieves a balance of angular momentum. The propagation directions derived fro m the two independent data sources agree in remarkable detail, and man y dynamical features can be identified, including the South Atlantic C urrent and the Tasman Front. The wavelengths calculated using the two data sets are quite sensitive to details of the processing. While this means they can be said to be ''not inconsistent,'' the relationship b etween temperature gradients and slopes demands further investigation. The results on direction of propagation, however, are robust.