Influence of waves on the three-dimensional distribution of plastic in the ocean

The world's oceans are facing plastic pollution, 80 % of which of terrestrial origin flowing from the mismanaged waste of coastal populations and from river discharge. To study the fate of this pollution, the three-dimensional trajectories of neutral plastic particles continuously released for...

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Veröffentlicht in:Marine pollution bulletin 2023-02, Vol.187, p.114533-114533, Article 114533
Hauptverfasser: Bajon, Raphaël, Huck, Thierry, Grima, Nicolas, Maes, Christophe, Blanke, Bruno, Richon, Camille, Couvelard, Xavier
Format: Artikel
Sprache:eng
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Zusammenfassung:The world's oceans are facing plastic pollution, 80 % of which of terrestrial origin flowing from the mismanaged waste of coastal populations and from river discharge. To study the fate of this pollution, the three-dimensional trajectories of neutral plastic particles continuously released for 24 years according to realistic source scenarios are computed using currents from a global ocean-wave coupled model at 14∘ resolution and from a reference ocean-only model. These Lagrangian simulations show that neutral particles accumulate at the surface in the subtropical convergence zones from where they penetrate to about 250 m depth and strongly disperse over 40∘ of latitude. About 5.3 % of the particles remain at the surface with the wave-coupled model currents, whereas only 2 % for the uncoupled model, with some modulation in the location of the convergence zones. Increased surface retention results from upward vertical velocities induced by widespread divergence of waves-induced Stokes transport in the surface layers. •Land-based scenario considers plastic waste from coastal populations or brought by rivers.•3D global dispersion of neutral ‘plastic’ particles in the global ocean•Coupled ocean-wave dynamics increase the surface retention of plastic by a factor of•Shapes of the concentrated plastic areas change when coupling with waves.•Ocean-wave coupling induces upward velocities below subtropical convergence zones.
ISSN:0025-326X
1879-3363
DOI:10.1016/j.marpolbul.2022.114533