Combining Litter Observations with a Regional Ocean Model to Identify Sources and Sinks of Floating Debris in a Semi-enclosed Basin: The Adriatic Sea

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dc.contributor.author Carlson, Daniel F.
dc.contributor.author Suaria, Giuseppe
dc.contributor.author Aliani, Stefano
dc.contributor.author Fredj, Erick
dc.contributor.author Fortibuoni, Tomaso
dc.contributor.author Griffa, Annalisa
dc.contributor.author Russo, Aniello
dc.contributor.author Melli, Valentina
dc.date.accessioned 2019-07-25T08:20:38Z
dc.date.available 2019-07-25T08:20:38Z
dc.identifier.uri http://hdl.handle.net/11201/149715
dc.description.abstract [eng] Visual ship transect surveys provide crucial information about the density, and spatial distribution of floating anthropogenic litter in a basin. However, such observations provide a 'snapshot' of local conditions at a given time and cannot be used to deduce the provenance of the litter or to predict its fate, crucial information for management and mitigation policies. Particle tracking techniques have seen extensive use in these roles, however, most previous studies have used simplistic initial conditions based on bulk average inputs of debris to the system. Here, observations of floating anthropogenic macro debris in the Adriatic Sea are used to define initial conditions (number of particles, location, and time) in a Lagrangian particle tracking model. Particles are advected backward and forward in time for 60 days (120 days total) using surface velocities from an operational regional ocean model. Sources and sinks for debris observed in the central and southern Adriatic in May 2013 and March 2015 included the Italian coastline from Pescara to Brindisi, the Croatian island of Mljet, and the coastline from Dubrovnik through Montenegro to Albania. Debris observed in the northern Adriatic originated from the Istrian peninsula to the Italian city of Termoli, as well as the Croatian island of Cres and the Kornati archipelago. Particles spent a total of roughly 47 days afloat. Coastal currents, notably the eastern and western Adriatic currents, resulted in large alongshore displacements. Our results indicate that anthropogenic macro debris originates largely from coastal sources near population centers and is advected by the cyclonic surface circulation until it strands on the southwest (Italian) coast, exits the Adriatic, or recirculates in the southern gyre.
dc.format application/pdf
dc.relation.isformatof Reproducció del document publicat a: https://doi.org/10.3389/fmars.2017.00078
dc.relation.ispartof Frontiers in Marine Science, 2017, vol. 4, num. 78, p. 1-16
dc.rights cc-by (c) Carlson, Daniel F. et al., 2017
dc.rights.uri http://creativecommons.org/licenses/by/3.0/es
dc.subject.classification 5 - Ciències pures i naturals
dc.subject.other 5 - Mathematical and Natural Sciences
dc.title Combining Litter Observations with a Regional Ocean Model to Identify Sources and Sinks of Floating Debris in a Semi-enclosed Basin: The Adriatic Sea
dc.type info:eu-repo/semantics/article
dc.type info:eu-repo/semantics/publishedVersion
dc.date.updated 2019-07-25T08:20:38Z
dc.rights.accessRights info:eu-repo/semantics/openAccess
dc.identifier.doi https://doi.org/10.3389/fmars.2017.00078


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cc-by (c) Carlson, Daniel F. et al., 2017 Except where otherwise noted, this item's license is described as cc-by (c) Carlson, Daniel F. et al., 2017

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