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  1. Abstract. New possibilities for horizontal current retrieval inmarginal ice zones (MIZs) from sequential Sentinel-1 synthetic apertureradar (SAR) images are demonstrated. Daily overlapping SAR acquisitionswithin 70–85∘ S/N at time intervals < 1 h enableestimation of high-resolution velocity fields, revealing MIZ dynamics downto submesoscales. An example taken from the Fram Strait MIZ revealsenergetic eddies and filaments with Rossby numbers reaching O(1) magnitudes.The SAR-derived velocity estimations at such high spatial resolution can becritical for monitoring the evolving MIZ dynamics and model validation ofsubmesoscale processes in polar oceans. 
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  2. Abstract

    In the Arctic Ocean, limited measurements indicate that the strongest mixing below the atmospherically forced surface mixed layer occurs where tidal currents are strong. However, mechanisms of energy conversion from tides to turbulence and the overall contribution of tidally driven mixing to Arctic Ocean state are poorly understood. We present measurements from the shelf north of Svalbard that show abrupt isopycnal vertical displacements of 10–50 m and intense dissipation associated with cross‐isobath diurnal tidal currents of0.15 m s−1. Energy from the barotropic tide accumulated in a trapped baroclinic lee wave during maximum downslope flow and was released around slack water. During a 6‐hr turbulent event, high‐frequency internal waves were present, the full 300‐m depth water column became turbulent, dissipation rates increased by a factor of 100, and turbulent heat flux averaged 15 W m−2compared with the background rate of 1 W m−2.

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