Convergent flow at the foot of the shelfbreak front in the Middle Atlantic Bight has been detected using a dye tracer, Rhodamine-WT, injected into the bottom boundary layer. The observations substantiate model simulations by Chapman and Lentz (1994) of convergent flow in the vicinity of the front which would be very difficult if not impossible to detect with conventional moored current measurements. By following the dispersal of the dye patch over a 4 day period Lagrangian velocities of the order of 0.015 m/s with respect to the front were resolved even as the frontal boundary was displaced ~12 km onshore. The water-following properties of the dye tracer provides a useful technique for studying the small-scale circulation and mixing at the frontal boundary.¿ 1997 American Geophysical Union