Winter in the coastal ocean: Seasonal freezing causes seafloor expansion and contraction

Seafloor mapping in polar regions has led to the recognition of landforms associated with subsea permafrost. Despite recent studies indicating rapid subsea permafrost degradation, information on seasonal seafloor changes remains limited. Here, we use time-lapse multibeam bathymetry (2021-2024) and bottom-water temperature data to reveal seasonal formation and degradation of small frost blisters (5 meters wide and 20 to 50 centimeters high) as ice forms within surficial sediments. These frost blisters were degraded in October 2021 at depths of ≤25 meters but were widespread in July 2023. They thawed between July and November 2023, reformed over the following winter, and were present again in August 2024. Data from moored bottom-water sensors and sediment cores indicate that the formation and degradation of frost blisters are driven by seasonal temperature changes at depth and influenced by freshened porewater in surficial sediments. This study documents previously unrecognized seasonal expansion and contraction of the seafloor driven by freeze-thaw cycles of freshened porewater.

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Publication Details

Journal
Science Advances
Published
2025-10-29
DOI
https://doi.org/10.1126/sciadv.adw7439
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
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article

Winter in the coastal ocean: Seasonal freezing causes seafloor expansion and contraction

Christopher K. Algar, Robert G. Way, Frédéric Cyr, Audrey Limoges et al.
Science Advances
Climate change and permafrost
article

Winter in the coastal ocean: Seasonal freezing causes seafloor expansion and contraction

Christopher K. Algar, Robert G. Way, Frédéric Cyr, Audrey Limoges, Jordan B.R. Eamer, Emma Harrison, Barret L. Kurylyk, Ian Church, Eric C. J. Oliver, Nicolas Van Nieuwenhove, Zachary MacMillan-Kenny, G Philibert, Liz Pijogge, Jennifer Eamer, Alexandre Normandeau, Haley D. Geizer, Michelle Saunders
article en

Abstract

Seafloor mapping in polar regions has led to the recognition of landforms associated with subsea permafrost. Despite recent studies indicating rapid subsea permafrost degradation, information on seasonal seafloor changes remains limited. Here, we use time-lapse multibeam bathymetry (2021-2024) and bottom-water temperature data to reveal seasonal formation and degradation of small frost blisters (5 meters wide and 20 to 50 centimeters high) as ice forms within surficial sediments. These frost blisters were degraded in October 2021 at depths of ≤25 meters but were widespread in July 2023. They thawed between July and November 2023, reformed over the following winter, and were present again in August 2024. Data from moored bottom-water sensors and sediment cores indicate that the formation and degradation of frost blisters are driven by seasonal temperature changes at depth and influenced by freshened porewater in surficial sediments. This study documents previously unrecognized seasonal expansion and contraction of the seafloor driven by freeze-thaw cycles of freshened porewater.

Science AdvancesVol. 11(44)
University of New Brunswick (CA), Dalhousie University (CA), Memorial University of Newfoundland (CA), Fisheries and Oceans Canada (CA), Bedford Institute of Oceanography (CA), Geoscience BC (CA), Government of Nunavut (CA)
Openalex Percentile: Top 63%
Climate change and permafrost
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