Time series analyses of current meter records from a 6-element box array installed on the narrow shelf (<5 km) off Miami, Florida revealed two distinct current regimes. Current oscillations at the shelf break (30m isobath) appeared to be primarily produced by Florida Current spawned events, such as low frequency (periods of 2 days to 2 weeks) wave-like meanders of the Florida Current and the transient occurrence of small diameter spin-off eddies, both of which may be indirectly related to wind forcing....