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Editorial: Marine Litter Windrows

Authors :
Stefano Aliani
Oihane C. Basurko
Manuel Arias
Atsuhiko Isobe
Anna Rubio
Konstantinos Topouzelis
Andrés Cózar
Agencia Estatal de Investigación (España)
Fundación BBVA
Ministerio de Economía y Competitividad (España)
Environment Research and Technology Development Fund
Ministry of the Environment (Japan)
Japan International Cooperation Agency
Japan Science and Technology Agency
Source :
Frontiers in Marine Science, Vol 8 (2022), Digital.CSIC. Repositorio Institucional del CSIC, instname
Publication Year :
2022
Publisher :
Frontiers Media S.A., 2022.

Abstract

3 pages<br />Our civilization produced about 8,300 Mt of synthetic polymers to date (Geyer et al., 2017), and the seas and oceans are pooling much of them (González-Fernández et al., 2021). Figuring out how all this marine litter moves and where it accumulates is a challenging task (Van Sebille et al., 2020). In some cases, we have been able to describe the distribution of plastics at a large-scale and associated to steady circulation patterns (e.g., Cózar et al., 2014), but understanding plastic distribution at small scale is more complex, due to the also complex ocean dynamics at such scales, and the much shorter-lived structures resulting from it. Actually, if we look at the ocean surface, it is common to see floating natural and man-made materials aggregated in small dense patches, often arranged in parallel lines sometime more than one kilometer long. They are traditionally called windrows in the scientific literature (Faller and Woodcock, 1964; Owen, 1965; Craik, 1970; Leibovich, 1983); foam lines, slicks, drift lines, rip lines, filaments, or streaks are synonyms. There is no definitive classification, but a listing of them would include windrows generated by tidal fronts, shelf-break fronts, upwelling fronts, river plumes, estuarine fronts, fronts associated with the convergence or divergence of water masses in the open ocean, frontal eddies, caused by internal waves, and fronts associated with geomorphologic features such as headlands, islands, and canyons (Mann and Lazier, 2006). All these processes are capable to create the surface evidence that we call windrows. In this volume, some aspects of ocean windrows are presented, focusing on the interaction of windrows with marine debris and related problems and opportunities. [...]<br />This editorial is an outcome of the following research projects: ESA WASP, ESA PLP, PRIN WERYZP EMME, JPI Oceans FACTS, PNRA IPSODES, PLASTREND (BBVA Foundation) and MIDaS (CTM2016-77106-R, AEI/FEDER/UE), JERICO-S3, LIFE LEMA, Environmental Research and Technology Development Fund (JPMEERF18S20201) of the Ministry of the Environment, Japan, and SATREPS of Japan International Cooperation Agency and Japan Science and Technology Agency. [...] With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S)

Details

Language :
English
ISSN :
22967745
Volume :
8
Database :
OpenAIRE
Journal :
Frontiers in Marine Science
Accession number :
edsair.doi.dedup.....8616f9fdff9bcae7a6ff9aa5b9f1bde0