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- Title
Effects of Eulerian current, Stokes drift and wind while simulating surface drifter trajectories in the Baltic Sea.
- Authors
Pärn, Ove; Davulienė, Lina; Macias Moy, Diego; Vahter, Kaimo; Stips, Adolf; Torsvik, Tomas
- Abstract
• Stokes drift has a strong impact on the simulation of the observed drifters, • For Lagrangian simulations in mean and low wave conditions, it is sufficient to use only the Eulerian currents and the windage factor. • The Lagrangian model is reliable for marine litter simulation, The simulation of Lagrangian drift is an important task in applications such as dispersion of pollutants, larvae and search and rescue activities. In this study, the Eulerian current, Stokes drift and wind effect on the simulation of observed drifters were analysed. The Lagrangian OceanParcels model was used, and the surface trajectories were assessed by comparison with 9 GPS drifter trajectories in the Gulf of Finland, Gulf of Riga and Lithuanian coast. The Normalised Cumulative Lagrangian Separation (NCLS) distance between the simulated and the satellite-tracked drifter trajectories, and the mean absolute error (MAE) were used as comparison metrics. The present study suggests the need to consider the Stokes drift and the wind factor in addition to the modelled Eulerian currents to obtain a better description of the trajectories of particles. By making these considerations, the OceanParcels model could adequately simulate particle trajectories in the sub-basins within the Baltic Sea. The realized model tests showed that motion of surface drifters are strongly controlled by the Stokes drift when the significant wave height is >1 m, whereas the wind component and the Eulerian currents are crucial when the significant wave height is <0.6 m or the wave (Stokes drift) directions do not match the wind direction.
- Subjects
GULF of Finland; MARINE debris; PARTICLE tracks (Nuclear physics); RESCUE work; POLLUTANTS; LARVAE
- Publication
Oceanologia, 2023, Vol 65, Issue 3, p453
- ISSN
0078-3234
- Publication type
Article
- DOI
10.1016/j.oceano.2023.02.001