Abstract:Sea ice dynamics span a wide range of scales and exhibit granular behavior as individual floes and fracture networks become evident at length scales O(10--100) km and smaller. Existing floe-scale sea ice models use bonded elements of predefined simple shapes like disks or tetrahedra to represent more complex floe geometries. However, floe-scale modeling remains challenging due to its typically high computational cost and difficulties in reconciling the idealized nature of discrete elements with complex floe-sc… Show more
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