Discrete-element model for the interaction between ocean waves and sea ice

TL;DR

This paper introduces a discrete element model to simulate how ocean waves cause sea ice to fracture and fragment, providing insights into ice breakup processes and fragment size distribution.

Contribution

The paper presents a novel DEM approach modeling sea ice as bonded particles, explicitly capturing fracture behavior due to wave interactions, which was not previously modeled in this detail.

Findings

Broken bond fraction increases with wave amplitude

Ice fragment size decreases as wave amplitude increases

Model provides spatial and temporal stress distribution data

Abstract

We present a discrete element method (DEM) model to simulate the mechanical behavior of sea ice in response to ocean waves. The interaction of ocean waves and sea ice can potentially lead to the fracture and fragmentation of sea ice depending on the wave amplitude and period. The fracture behavior of sea ice is explicitly modeled by a DEM method, where sea ice is modeled by densely packed spherical particles with finite size. These particles are bonded together at their contact points through mechanical bonds that can sustain both tensile and compressive forces and moments. Fracturing can be naturally represented by the sequential breaking of mechanical bonds. For a given amplitude and period of incident ocean wave, the model provides information for the spatial distribution and time evolution of stress and micro-fractures and the fragment size distribution. We demonstrate that the fraction of broken bonds, , increases with increasing wave amplitude. In contrast, the ice fragment size l decreases with increasing amplitude. This information is important for the understanding of breakup of individual ice floes and floe fragment size.