Evidence of upwelling events at the northern Patagonian shelf break

The Patagonian shelf break marks a transition between relative warm-fresh shelf waters and relative cold-salty Subantarctic Water advected northward by the Malvinas Current. From early spring to late autumn, the outer shelf region is characterized by a band of high chlorophyll concentration that sus...

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Detalles Bibliográficos
Publicado:	2015
Materias:	Malvinas Current ocean currents shelf break South Atlantic upwelling advection chlorophyll a cooling mixed layer mooring system nutrient cycling oceanic current phytoplankton satellite data sea surface temperature time series analysis transition zone trophic level water exchange water mass Atlantic Ocean Atlantic Ocean (South) Patagonia
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_21699275_v120_n11_p7635_Valla http://hdl.handle.net/20.500.12110/paper_21699275_v120_n11_p7635_Valla
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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