Abstract
During the summer of 1994, a satellite‐tracked drifter transited from the southeastern Bering Sea slope through Bering Strait by a route westward along the slope and then northward through Anadyr Canyon and Strait. 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.
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