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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=19526"><dc:title>Lagrangian modelling of a person lost at sea during the Adriatic scirocco storm of 29 October 2018</dc:title><dc:creator>Ličer,	Matjaž	(Avtor)
	</dc:creator><dc:creator>Estival,	Solène	(Avtor)
	</dc:creator><dc:creator>Reyes-Suarez,	Catalina	(Avtor)
	</dc:creator><dc:creator>Deponte,	Davide	(Avtor)
	</dc:creator><dc:creator>Fettich,	Anja	(Avtor)
	</dc:creator><dc:description>On 29 October 2018 a windsurfer's mast broke about 1 km offshore from Istria during a severe scirocco storm in the northern Adriatic Sea. He drifted in severe marine conditions until he eventually beached alive and well in Sistiana (Italy) 24 h later. We conducted an interview with the survivor to reconstruct his trajectory and to gain insight into his swimming and paddling strategy. Part of survivor's trajectory was verified using high-frequency radar surface current observations as inputs for Lagrangian temporal back-propagation from the beaching site. Back-propagation simulations were found to be largely consistent with the survivor's reconstruction. We then attempted a Lagrangian forward-propagation simulation of his trajectory by performing a leeway simulation using the OpenDrift tracking code using two object types: (i) person in water in unknown state and (ii) person with a surfboard. In both cases a high-resolution (1 km) setup of the NEMO v3.6 circulation model was employed for the surface current component, and a 4.4 km operational setup of the ALADIN atmospheric model was used for wind forcing. The best performance is obtained using the person-with-a-surfboard object type, giving the highest percentage of particles stranded within 5 km of the beaching site. Accumulation of particles stranded within 5 km of the beaching site saturates 6 h after the actual beaching time for all drifting-particle types. This time lag most likely occurs due to poor NEMO model representation of surface currents, especially in the final hours of the drift. A control run of wind-only forcing shows the poorest performance of all simulations. This indicates the importance of topographically constrained ocean currents in semi-enclosed basins even in seemingly wind-dominated situations for determining the trajectory of a person lost at sea.</dc:description><dc:date>2020</dc:date><dc:date>2024-07-19 03:43:21</dc:date><dc:type>Neznano</dc:type><dc:identifier>19526</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
