The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris

Understanding the physical mechanisms behind the transport and accumulation of floating objects in the ocean is crucial to efficiently tackle the issue of marine pollution. The main sinks of marine plastic are the coast and the bottom sediment. This study focuses on the former, investigating the tim...

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Published in:Frontiers in Marine Science
Main Authors: Bosi, Sofia, Broström, Göran, Roquet, Fabien
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2021
Subjects:
Online Access:http://dx.doi.org/10.3389/fmars.2021.697430
https://www.frontiersin.org/articles/10.3389/fmars.2021.697430/full
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spelling crfrontiers:10.3389/fmars.2021.697430 2024-06-23T07:55:15+00:00 The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris Bosi, Sofia Broström, Göran Roquet, Fabien 2021 http://dx.doi.org/10.3389/fmars.2021.697430 https://www.frontiersin.org/articles/10.3389/fmars.2021.697430/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Marine Science volume 8 ISSN 2296-7745 journal-article 2021 crfrontiers https://doi.org/10.3389/fmars.2021.697430 2024-06-11T04:08:54Z Understanding the physical mechanisms behind the transport and accumulation of floating objects in the ocean is crucial to efficiently tackle the issue of marine pollution. The main sinks of marine plastic are the coast and the bottom sediment. This study focuses on the former, investigating the timescales of dispersal from the ocean surface and onto coastal accumulation areas through a process called “beaching.” Previous studies found that the Stokes drift can reach the same magnitude as the Eulerian current speed and that it has a long-term effect on the trajectories of floating objects. Two particle tracking models (PTMs) are carried out and then compared, one with and one without Stokes drift, named PTM-SD and PTM-REF , respectively. Eulerian velocity and Stokes drift data from global reanalysis datasets are used for particle advection. Particles in the PTM-SD model are found to beach at a yearly rate that is double the rate observed in PTM-REF . The main coastal attractors are consistent with the direction of large-scale atmospheric circulation (Westerlies and Trade Winds). After 12 years (at the end of the run), the amount of beached particles is 20% larger in PTM-SD than in PTM-REF . Long-term predictions carried out with the aid of adjacency matrices found that after 100 years all particles have beached in PTM-SD , while 8% of the all seeded particles are still floating in PTM-REF . The results confirm the need to accurately represent the Stokes drift in particle models attempting to predict the behaviour of marine debris, in order to avoid overestimation of its residence time in the ocean and effectively guide policies toward prevention and removal. Article in Journal/Newspaper North Atlantic Frontiers (Publisher) Frontiers in Marine Science 8
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
description Understanding the physical mechanisms behind the transport and accumulation of floating objects in the ocean is crucial to efficiently tackle the issue of marine pollution. The main sinks of marine plastic are the coast and the bottom sediment. This study focuses on the former, investigating the timescales of dispersal from the ocean surface and onto coastal accumulation areas through a process called “beaching.” Previous studies found that the Stokes drift can reach the same magnitude as the Eulerian current speed and that it has a long-term effect on the trajectories of floating objects. Two particle tracking models (PTMs) are carried out and then compared, one with and one without Stokes drift, named PTM-SD and PTM-REF , respectively. Eulerian velocity and Stokes drift data from global reanalysis datasets are used for particle advection. Particles in the PTM-SD model are found to beach at a yearly rate that is double the rate observed in PTM-REF . The main coastal attractors are consistent with the direction of large-scale atmospheric circulation (Westerlies and Trade Winds). After 12 years (at the end of the run), the amount of beached particles is 20% larger in PTM-SD than in PTM-REF . Long-term predictions carried out with the aid of adjacency matrices found that after 100 years all particles have beached in PTM-SD , while 8% of the all seeded particles are still floating in PTM-REF . The results confirm the need to accurately represent the Stokes drift in particle models attempting to predict the behaviour of marine debris, in order to avoid overestimation of its residence time in the ocean and effectively guide policies toward prevention and removal.
format Article in Journal/Newspaper
author Bosi, Sofia
Broström, Göran
Roquet, Fabien
spellingShingle Bosi, Sofia
Broström, Göran
Roquet, Fabien
The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
author_facet Bosi, Sofia
Broström, Göran
Roquet, Fabien
author_sort Bosi, Sofia
title The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
title_short The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
title_full The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
title_fullStr The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
title_full_unstemmed The Role of Stokes Drift in the Dispersal of North Atlantic Surface Marine Debris
title_sort role of stokes drift in the dispersal of north atlantic surface marine debris
publisher Frontiers Media SA
publishDate 2021
url http://dx.doi.org/10.3389/fmars.2021.697430
https://www.frontiersin.org/articles/10.3389/fmars.2021.697430/full
genre North Atlantic
genre_facet North Atlantic
op_source Frontiers in Marine Science
volume 8
ISSN 2296-7745
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fmars.2021.697430
container_title Frontiers in Marine Science
container_volume 8
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