Seasonal evolution of the sea ice floe size distribution in the Beaufort Sea from 2 decades of MODIS data

Abstract. Arctic sea ice cover evolves seasonally from large plates separated by long, linear leads in the winter to a mosaic of smaller sea ice floes in the summer. The interplay between physical and thermodynamic mechanisms during this process ultimately creates the observed sea ice floe size distribution (FSD), which is an important metric for characterizing the sea ice cover and assessing model performance. Historically, the FSD has been studied at fixed locations over short periods, leaving a gap in our understanding of the spatial and temporal evolution of the FSD at large scales. Here, we present an automated framework for image segmentation, allowing the identification and labeling of individual ice floes in Moderate Resolution Imaging Spectroradiometer (MODIS) data. Using this algorithm, we automatically process and segment 4861 images, identifying more than 9.4 million floes over 23 years. The extracted characteristics of the floes – including area, perimeter, and orientation – evolve throughout the spring and summer in the Beaufort Sea. We find seasonal patterns of decreasing mean floe areas, increasing FSD power law slopes, and increasing variability in the floe orientation as the summer progresses.

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Publication Details

Journal
˜The œcryosphere
Published
2024-11-06
DOI
https://doi.org/10.5194/tc-18-5031-2024
Citations
5
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.88

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article

Seasonal evolution of the sea ice floe size distribution in the Beaufort Sea from 2 decades of MODIS data

Mary‐Louise Timmermans, Monica M. Wilhelmus, Leela Cañuelas, Ellen Buckley
5 citations
˜The œcryosphere
Arctic and Antarctic ice dynamics
1.88
article

Seasonal evolution of the sea ice floe size distribution in the Beaufort Sea from 2 decades of MODIS data

Mary‐Louise Timmermans, Monica M. Wilhelmus, Leela Cañuelas, Ellen Buckley
article en
5 citations

Abstract

Abstract. Arctic sea ice cover evolves seasonally from large plates separated by long, linear leads in the winter to a mosaic of smaller sea ice floes in the summer. The interplay between physical and thermodynamic mechanisms during this process ultimately creates the observed sea ice floe size distribution (FSD), which is an important metric for characterizing the sea ice cover and assessing model performance. Historically, the FSD has been studied at fixed locations over short periods, leaving a gap in our understanding of the spatial and temporal evolution of the FSD at large scales. Here, we present an automated framework for image segmentation, allowing the identification and labeling of individual ice floes in Moderate Resolution Imaging Spectroradiometer (MODIS) data. Using this algorithm, we automatically process and segment 4861 images, identifying more than 9.4 million floes over 23 years. The extracted characteristics of the floes – including area, perimeter, and orientation – evolve throughout the spring and summer in the Beaufort Sea. We find seasonal patterns of decreasing mean floe areas, increasing FSD power law slopes, and increasing variability in the floe orientation as the summer progresses.

˜The œcryosphereVol. 18(11)
Planetary Science Institute (US), Brown University (US), Yale University (US)
Office of Naval Research
Life below water
Openalex Percentile: Top 15%
Arctic and Antarctic ice dynamics
1.88
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Seasonal evolution of the sea ice floe size distribution in the Beaufort Sea from 2 decades of MODIS data — Mary‐Louise Timmermans, Monica M. Wilhelmus, et al. · ˜The œcryosphere (2024) | TGRS Research Map | TGRS