Wind waves in sea ice of the western Arctic and a global coupled wave-ice model

• Published in: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
• Main Authors: Cooper, V. T., Roach, L. A., Thomson, J., Brenner, S. D., Smith, M. M., Meylan, M. H., Bitz, C. M.
• Other Authors: Office of Naval Research, New Zealand Ministry of Business, Innovation and Employment, National Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: The Royal Society 2022
• Subjects: General Physics and Astronomy; General Engineering; General Mathematics; Antarc*; Antarctic; Sea ice
• Online Access: http://dx.doi.org/10.1098/rsta.2021.0258; https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2021.0258; https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2021.0258

The retreat of Arctic sea ice is enabling increased ocean wave activity at the sea ice edge, yet the interactions between surface waves and sea ice are not fully understood. Here, we examine in situ observations of wave spectra spanning 2012–2021 in the western Arctic marginal ice zone (MIZ). Swells exceeding 30 cm are rarely observed beyond 100 km inside the MIZ. However, local wind waves are observed in patches of open water amid partial ice cover during the summer. These local waves remain fetch-limited between ice floes with heights less than 1 m. To investigate these waves at climate scales, we conduct experiments varying wave attenuation and generation in ice with a global model including coupled interactions between waves and sea ice. A weak high-frequency attenuation rate is required to simulate the local waves in observations. The choices of attenuation scheme and wind input in ice have a remarkable impact on the extent of wave activity across ice-covered oceans, particularly in the Antarctic. As well as demonstrating the need for stronger constraints on wave attenuation, our results suggest that further attention should be directed towards locally generated wind waves and their role in sea ice evolution. This article is part of the theme issue ‘Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks’.