“…This feature, which is evident along the entire southeastern shelf, limits the horizontal flux of salt, nutrients and heat between the middle and coastal domains (Coachman, 1986;Kachel et al, 2002). A similar feature occurs around the Pribilof Islands, where it enhances feeding opportunities for higher trophic level organisms (Kinder, Hunt, Schneider & Schumacher, 1983;Decker & Hunt, 1996;Hunt, Coyle, Hoffman, Decker & Flint, 1996a;Brodeur, Wilson & Ciannelli, 2000).…”