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Persistency and Surface Convergence Evidenced by Two Maker Buoys in the Great Pacific Garbage Patch

Journal of Marine Science and Engineering 2023 4 citations ? Citation count from OpenAlex, updated daily. May differ slightly from the publisher's own count. Score: 35 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Bruno Sainte-Rose, Yannick Pham, Wayne J. Pavalko

Summary

Researchers tracked two drifting buoys released in the Great Pacific Garbage Patch in 2019 and compared their trajectories to circulation divergence fields, Lagrangian plastic dispersal models, and sea-level anomalies, demonstrating that persistent negative velocity divergence and elevated modelled plastic surface density coincide with surface convergence zones that concentrate floating debris.

Study Type Environmental

The accumulation of plastic debris on land and coastlines and in waterways and garbage patches is one of the greatest ecological concerns of the 21st century. In that context, the sources and pathways of plastic marine debris (PMD) have been increasingly studied in the past ten years. The purpose of this communication was to analyze, thanks to the tracks of two drifting buoys released in May–June 2019 in the North-East Pacific, two features encountered within the Great Pacific Garbage Patch (GPGP): a surface convergence, which could lead to the formation of plastic hotspots, and the persistency of the floating material in this area of the ocean. The evolution of the distance between the buoys was compared with the local circulation field divergence, a Lagrangian plastic dispersal model and sea-level anomalies (SLAs). These analyses highlighted the link between the converging behavior of the drifters and a persistent negative velocity divergence as well as a higher than average-encountered modelled plastic surface density (MPSD). The persistence of the material within the GPGP was observed thanks to the trajectory of the longest persisting drifter in comparison with the trajectory of the GPGP center and extent.

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