Flow of Ice Through Converging Channels

摘要

This paper presents a study of the flow of ice in wedge-shaped converging channels. Such flows are encountered in the relatively constricted waters of the Canadian Arctic Archipelago. Ridging, lead opening patterns, development of a high-pressure area, and arch formation are some of the processes which take place during ice flow through converging channels. An idealized geometry and steady wind forcing were used in the testing. The results give ice cover velocity, distribution of stresses, ice thickness, area coverage and ridging. Some of the conditions leading to arch formation at the constricted exit of the channel are explored.