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Siobhan P. O’Farrell on Muck Rack

Siobhan P. O’Farrell

As seen in: Nature, Wiley Online Library, Weather and Forecasting
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Articles

Revealing the Antarctic marginal ice zone with a decade-long wave-in-ice climatology

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By Alexander Fraser, Noah Day, Zhaohui Wang, Luke Bennetts, Qingxiang Liu, Siobhan P. O’Farrell, Richard Coleman, Joey J. Voermans, Shiming Xu, Weixin Zhu, Matthis Auger, Robert Massom, Pat Wongpan, Takenobu Toyota, Petra Heil, Christopher Horvat, Lisa Craw, Jill Brouwer
| Nature Verified
Abstract The marginal ice zone (MIZ) is the region of sea ice that is strongly influenced by open-ocean processes, particularly ocean waves. The width of the Antarctic MIZ is often quantified by applying thresholds to satellite-derived maps of sea-ice concentration, although this definition lacks any connection to waves. Laser altimetry provides snapshots of wave penetration, but is restricted by cloud cover.
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Analysis of the Antarctic Marginal Ice Zone Based on Unsupervised Classification of Standalone Sea Ice Model Data

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By Noah Day, Luke Bennetts, Alberto Alberello, Siobhan P. O’Farrell
| Wiley Online Library Verified
1 Introduction The Antarctic marginal ice zone (MIZ) is the region at the outer margins of the sea ice covered Southern Ocean, where the ice cover is regularly affected by ocean-surface waves, as well as other open-ocean processes (Bennetts et al., 2022b; Wadhams, 1986).
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