GULF-STREAM PATH AND THERMOCLINE STRUCTURE NEAR 74-DEGREES-W AND 68-DEGREES-W

The SYNoptic Ocean Prediction.(SYNOP) experiment had the goal of Providing a physical understanding of energetic mesoscale eddy processes in the Gulf Stream. In the SYNOP Inlet Array off Cape Hatteras and in the Central Array near 68 degrees W moored observations were collected from October 1987 through August 1990. The Inlet Array measured the surface path and bottom currents where the Gulf Stream leaves the continental margin to enter the deep water regime; small amplitude propagating and growing meanders characterized the variability there. The Central Array measured velocity and temperature (as a proxy for density) at four levels in the water column, as well as the upper and deep level streamfunctions, all with mesoscale resolution. Near 70 degrees W the path envelope exhibited a relative node, confined within a 40-km band 55% of the time. Near 68 degrees W the path envelope was over 3 times as wide, due to several elongated (''steep'') meander troughs and relatively steep meander crests. The crests typically propagated downstream without much growth. The troughs often stalled near 68 degrees W, steepened, and persisted for one to several months. Two cases evolved into ''S-shaped'' paths and subsequently formed rings. Even the time-averaged fields showed a small trough in the mean path and thermocline structure. Whereas meanders df 20- to 60-day periods had similar spectral levels throughout 70 degrees-67 degrees W, meanders with long periods (> 85 day) accounted for the local minimum in variance at 70 degrees W. Bottom pressure and velocity observations revealed repeated periods of intense (swirl speeds > 0.30 m s(-1)) abyssal eddies; the time-averaged deep currents exhibited a mean cyclone centered 30 km offshore and downstream of the upper layer mean trough. The cross-stream slope of the thermocline steepened linearly with path curvature, consistent with gradient wind balance. Structures are illustrated in the mapped fields consistent with baroclinic instability wherein troughs steepen and rings form.