Evidence of episodic on-shelf flow in the southeastern Bering Sea

Trajectories from satellite-tracked drifters released over the continental slope (depth 250-500 m) in the southeastern Bering Sea revealed an episodic event of on-shelf flow. The first set of seven drifters followed the isoba ths northwestward at speeds of 20-40 cm s(-1); the second set, released 12 days later, moved 60 km onto the shelf at speeds of 10-15 cm s(-1). Meander s or eddies were evident in the trajectories as the drifters were advected onto the shelf. An anticyclonic eddy formed at the shoreward termination of on-shelf flow (120 m isobath). The eddy dissipated in 8-10 days. Such even ts can be important mechanisms in replenishing nutrients and introducing oc eanic plankton and larvae onto the shelf.