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Ocean waves have been observed to fracture sea ice in the Arctic and Southern Oceans, a process which is hypothesised to partially control sea ice extent. We proposed a new mathematical model to simulate the repeated breakup of an ice field into many floes with different sizes under sustained wave forcing. Although field measurements suggest that the resulting floe size distribution should obey a power law, we show that waves alone are unlikely to be responsible for this scaling characteristic. We further identify specific ice and wave conditions that lead to enhanced sea ice breakup caused by constructive wave interference.

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This page is a summary of: Modelling wave-induced sea ice break-up in the marginal ice zone, Proceedings of the Royal Society A Mathematical Physical and Engineering Sciences, October 2017, Royal Society Publishing,
DOI: 10.1098/rspa.2017.0258.
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