info:eu-repo/semantics/article
Dataset on the RETRO-BMC cruise onboard the R/V Hespérides, April 2017, Brazil-Malvinas Confluence
Fecha
2020-06Registro en:
Orúe Echevarría, Dorleta; Pelegrí, Josep L.; Castellanos, Paola; Guallar, Carles; Marotta, Humberto; et al.; Dataset on the RETRO-BMC cruise onboard the R/V Hespérides, April 2017, Brazil-Malvinas Confluence; Elsevier; Data in Brief; 30; 6-2020; 1-16
2352-3409
CONICET Digital
CONICET
Autor
Orúe Echevarría, Dorleta
Pelegrí, Josep L.
Castellanos, Paola
Guallar, Carles
Marotta, Humberto
Marrasé, Cèlia
Martín de Nascimento, Jacobo
Masdeu Navarro, Marta
Paniagua, Guillermina Fernanda
Peña Izquierdo, Jesús
Puigdefábregas, Joan
Rodríguez Fonseca, Belén
Roget, Elena
Rosell Fieschi, Miquel
Salat, Jordi
Salvador, Joaquín
Vallès Casanova, Ignasi
Vidal, Montserrat
Viúdez, Álvaro
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.