High-resolution simulations of submesoscale processes in the Baltic Sea: The role of storm events

Recently discovered, ocean submesoscales have attracted considerable attention due to their ability to change the upper ocean stratification, affect vertical transport, and induce a downscale cascade of energy toward dissipation. Here, we highlight the effect of submesoscale fronts and filaments on surface layer properties and dynamics during storm events, extending previous idealized simulations toward real-ocean applications. We use the Baltic Sea as a natural laboratory to study the rich submesoscale activity of this system with the help of realistic high-resolution numerical simulations. These simulations reveal a wealth of cold submesoscale filaments characterized by sharp lateral buoyancy gradients, strong surface convergence, and high vertical velocities. We show that highly heterogeneous Mixed Layer Depth (MLD) modulations are associated with these features, maintaining locally reduced MLDs even during storm events due to vigorous submesoscale restratification. The interaction of near-surface turbulence and submesoscale restratification results in strong and highly efficient mixing inside the submesoscale fronts.&nbsp
The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)