During the summer of 1994 a satellite-tracked drifter transited from t
he southeastern Bering Sea slope through Bering Strait by a route west
ward along the slope and then northward through Anadyr Canyon and Stra
it. The trajectory emphasizes the importance of a western location of
northward flow on the Bering Sea shelf. The transit time was 2 months
from Cape Navarin to Bering Strait with northward drift velocities of
5-40 cm/s.