Articles | Volume 20, issue 6
https://doi.org/10.5194/tc-20-3271-2026
https://doi.org/10.5194/tc-20-3271-2026
Research article
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09 Jun 2026
Research article | Highlight paper |  | 09 Jun 2026

The influence of ocean waves on Antarctic sea-ice albedo and seasonal melting, and potential coupled physical and biological feedbacks

Robert A. Massom, Phillip A. Reid, Stephen G. Warren, Bonnie Light, Donald K. Perovich, Luke G. Bennetts, Petteri Uotila, Siobhan P. O'Farrell, Michael H. Meylan, Klaus M. Meiners, Pat Wongpan, Alexander D. Fraser, Alessandro Toffoli, Giulio Passerotti, Peter G. Strutton, Sean M. T. Chua, and Melissa Fedrigo

Data sets

Calculation of Antarctic sea ice melt rate enhancements for "The influence of ocean waves on Antarctic sea-ice albedo and seasonal melting, and physical-biological feedbacks" Phillip Reid https://doi.org/10.5281/zenodo.18995070

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Editorial statement
This manuscript is relevant for the broader geoscience community and the broader public/media as it discusses in depth the role of waves in ice that goes beyond commonly considered mechanical break up but includes implications for radiation, melting, and biology, and the feedbacks thereof. It thus also discusses critical missing processes in climate models. The manuscript includes recommendations for future research focused in the role of waves in ice that will direct future research projects and cruises. Compelling visuals make the material particularly accessible for a broader public.
Short summary
This paper advances understanding of why and how Antarctic sea ice can retreat so rapidly each summer, and identifies critical gaps in climate models, by highlighting 3 previously-neglected wave-driven processes and 5 associated feedbacks that accelerate seasonal ice melting and link physics to biology (wave flooding, wave pulverisation and wave greening). There are major implications for Earth’s radiation budget, Antarctic ecosystems and the accuracy of future sea-ice and climate projections.
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