Stepwise Subduction Observed at a Front in the Marginal Ice Zone in Fram Strait

At high latitudes, submesoscale dynamics act on scales of O $\mathcal{O}$(100 m–1 km) and are associated with the breakdown of geostrophic balance, vertical velocities, and energy cascading to small scales. Submesoscale features such as fronts, filaments, and eddies are ubiquitous in marginal ice zones forced by the large horizontal density gradients. In July 2020, we identified multiple fronts and filaments using a towed undulating vehicle near the sea ice edge in central Fram Strait, the oceanic gateway to the Arctic Ocean between Greenland and Svalbard. Sea ice covered the entire study region 1–2 weeks earlier, and a stratified meltwater layer was present. We observed a front between warm and saline Atlantic Water (AW) and cold and fresh Polar Water (PW) at 30–85 m depth, where we identified a subsurface maximum in chlorophyll fluorescence and other biogeochemical properties extending along the tilted isopycnals down to 75 m, indicating subduction of AW (mixed with meltwater) that had previously occurred. The meltwater layer also featured multiple shallow fronts, one of which exhibited high velocities and a subsurface maximum in chlorophyll fluorescence, possibly indicating subduction of PW below the meltwater layer. The fronts at different depth levels suggest a stepwise subduction process near the ice edge, where water subducts from the surface below the meltwater and then further down along subsurface fronts. The submesoscale features were part of a larger‐scale mesoscale pattern in the marginal ice zone. As sea ice continuously retreats, such features may become more common in the Arctic Ocean. Plain Language Summary Submesoscale dynamics are small‐scale (100 m–1 km) horizontal and vertical flows that create fronts and whirls. These features are typical in the transition from open ocean to sea ice. In the summer of 2020, we observed multiple fronts near the sea ice edge in central Fram Strait. Fram Strait is the oceanic gateway between the Atlantic Ocean and the Arctic Ocean. At the time, fresh meltwater covered the area. Below the meltwater layer, we observed a front between warm and saline Atlantic Water (AW) and cold and fresh Polar Water (PW). The amount of fluorescence (a measure of biomass) observed below the PW showed that AW moved downwards. Prior observations show that AW is in touch with the sea surface in the eastern part of Fram Strait. Our observations thus suggest a step‐by‐step process happening near the ice edge. AW moves from the su