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Preprints
https://doi.org/10.5194/essd-2025-14
https://doi.org/10.5194/essd-2025-14
06 Feb 2025
 | 06 Feb 2025
Status: this preprint is currently under review for the journal ESSD.

Satellite-based Analysis of Ocean-Surface Stress across the Ice-free and Ice-covered Polar Oceans

Chao Liu and Lisan Yu

Abstract. Ocean-surface stress is a critical driver of polar sea ice dynamics, air-sea interactions, and ocean circulation. This work provides a daily analysis of ocean-surface stress on 25-km Equal-Area Scalable Earth (EASE) Grids across the ice-free and ice-covered regions of the polar oceans (2011–2018 for Arctic, 2013–2018 for Antarctic), covering latitudes north of 60° N in the Arctic and south of 50° S in the Antarctic and Southern Ocean. Ocean-surface stress is calculated using a bulk parameterization approach that combines ocean-surface winds, ice motion vectors, and sea surface height (SSH) data from multiple satellite platforms. The analysis captures significant spatial and temporal variability in ocean-surface wind stress and the resultant wind-driven Ekman transport, while providing enhanced spatiotemporal resolution. Two sensitivity analyses are conducted to address key sources of uncertainty. The first addresses the fine-scale variability in SSH fields, which was mitigated using a 150-km Gaussian filter to smooth three-day SSH datasets and enhance compatibility with the other monthly product, followed by linear interpolation to achieve daily resolution. The second investigates uncertainty in the ice-water drag coefficient, which revealed that variations in the coefficient have a proportional influence on the computed ocean-surface stress under the tested conditions. These uncertainties are most pronounced during winter, with median values reaching 20 % in the Arctic and 40 % in the Southern Ocean. Validation efforts utilized Ice-Tethered Profiler velocity records, revealing moderate correlations (r = 0.6–0.8) at monthly timescales, effectively capturing low-frequency signals but with small northward biases. Satellite-derived velocity fields, including both Ekman and geostrophic components, explain 40–50 % of the total variance. The unexplained variance reflects unresolved processes, such as mesoscale dynamics and other unparameterized factors. This dataset is publicly available at https://doi.org/10.5281/zenodo.14750492 (Liu & Yu, 2024).

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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A daily dataset on ocean-surface stress is synthesized for both ice-covered and ice-free Arctic...
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