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
Autores principales: Valla, D., Piola, A.R.
Formato: JOUR
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: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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