| Summary: | Effects of surface gravity waves on particle transport and currents in the upper ocean are studied using field observations and numerical models. Knowledge on upper ocean particle drift is needed for plankton transport studies, search- and rescue operations and oil drift modelling. Such applications depend on upper ocean currents on time scales from hours up to several months, and surface gravity waves affect the air-sea momentum exchange particularly on these time scales. Objects near the surface are also exposed to the wave-induced Stokes drift, which moves particles in the wave propagation direction at a speed with similar magnitude as the Eulerian current. Surface waves furthermore modify the Eulerian mean currents by momentum release during wave breaking and the dissipation of wave energy into oceanic turbulence. Measurements of upper ocean currents, surface drifters, and waves were taken during field campaigns in Northern Norway. Ocean currents from acoustic Doppler current profilers, high-frequency (HF) radars and satellite-tracked surface drifters were synthesized with wave measurements to separate the Eulerian currents from the Lagrangian, their difference is the Stokes drift. The contribution of waves to surface drifter velocities and observed HF radar currents was quantified and compared with theoretical concepts from the literature. The surface drifters followed the sum of Eulerian currents and Stokes drift with little wind drag. In contrast to previous assumptions, the observation showed that HF radar-derived currents do not include the Stokes drift. The observations were also used to quantify the momentum and energy fluxes from waves into the ocean during a wind event. The wave-induced drift of suspended plankton was investigated for the example of Northeast Arctic (NEA) cod eggs. Their physical properties are relatively well known, providing a practical example for biological models that depend on oceanic circulation. A combined ocean circulation model, wave model and particle tracking model is ...
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