The Ocean Basin Model encourages experiments with ocean surface circulation in a homogeneous, rectangular ocean basin, driven by surface winds, ocean bottom friction, horizontal pressure gradients and the Coriolis force. (oceanmotion.org)
(i) Older, thicker multiyear ice continues to flush out of the high Canadian Arctic and depending on winter surface circulation, some of this ice may reach very close to the coast. (dotearth.blogs.nytimes.com)
Mean surface circulation is predominately cyclonic on the Eurasian side and anticyclonic in the Canadian Basin. (en.wikipedia.org)