Artículo

Dataset on the RETRO-BMC cruise onboard the R/V Hespérides, April 2017, Brazil-Malvinas Confluence

Orúe Echevarría, Dorleta Icon; Pelegrí, Josep L. Icon; Castellanos, Paola ; Guallar, Carles ; Marotta, Humberto ; Marrasé, Cèlia ; Martín de Nascimento, Jacobo Icon; Masdeu Navarro, Marta ; Paniagua, Guillermina Fernanda Icon; Peña Izquierdo, Jesús Icon; Puigdefábregas, Joan ; Rodríguez Fonseca, Belén ; Roget, Elena ; Rosell Fieschi, Miquel Icon; Salat, Jordi ; Salvador, Joaquín ; Vallès Casanova, Ignasi ; Vidal, Montserrat ; Viúdez, Álvaro

Otros responsables

Fecha

06/2020

Editorial

Elsevier

Revista

Data in Brief

Título del libro

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Fecha del evento

Institución organizadora

ISSN

2352-3409

eISSN

ISBN

Idioma

Inglés

Tipo del evento

Resumen

This dataset, gathered during the RETRO-BMC cruise, reports multiple-scale measurements at the Confluence of the Brazil and Malvinas Currents. The cruise was carried out between 8 and 28 April 2017 onboard R/V Hespérides, departing from Ushuaia and arriving to Santos. Along its track, the vessel recorded near-surface temperature and salinity, as well as the horizontal flow from 20 m down to about 800 m. A total of 33 hydrographic stations were completed in a region off the Patagonian Shelf, within 41.2°S–35.9°S and out to 53.0°W. At each station, a multiparametric probe and velocity sensors were deployed inside the frame of a rosette used to collect water samples at selected depths; these samples were later used for several water analyses, including inorganic nutrient concentrations. Microstructure measurements were carried out in 11 of these hydrographic stations. In addition, two high-resolution three-dimensional surveys were conducted with an instrumented undulating vehicle between 40.6°S–39.0°S and 55.6°W–53.8°W. Lastly, eight high-frequency vertical profilers were deployed in the region and five position-transmitting drifters were launched. These data allow the description of the Confluence from the regional scale to the microscale, and provide a view of the variability of the frontal region on time scales from days to weeks.

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