NPZ response to eddy-induced upwelling in a Brazil Current ring: A theoretical approach |
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| Affiliation: | 1. Departamento de Ecologia e Zoologia, Universidade Federal de Santa Catarina, Campus Universitário, 88040-970 Florianópolis, Brazil;2. Institut Français de Recherche pour l''Exploitation de la Mer, Centre de Bretagne, 1625 Route de Sainte-Anne, 29280 Plouzané, France;3. Instituto de Oceanografia, Universidade Federal do Rio Grande, Km 8 Avenida Itália, 96201-900 Rio Grande, Brazil;4. Programa de Pós-graduação em Oceanografia, Universidade Federal de Santa Catarina, Campus Universitário, 88040-970 Florianópolis, Brazil;1. Division of Earth and Ocean Sciences, Duke University, Durham, NC 27708, USA;2. Departamento de Geologia, Universidade Federal Fluminense, Niterói, RJ, Brazil;3. Department of Geological Sciences, East Carolina University, Greenville, NC 27858, USA;4. Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA;5. Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;6. Climate and Global Dynamics, National Center for Atmospheric Research, Boulder, CO 80307, USA;7. Department of Atmospheric and Oceanic Sciences, University of Wisconsin, Madison, WI 53706, USA;1. Programa de Pós-graduação em Geofísica, Instituto de Geociências, Universidade Federal da Bahia, Campus de Ondina, Travessa Barão de Jeremoabo, s/n, Salvador, BA, 40170-280, Brazil;2. Departamento de Física da Terra e do Meio Ambiente, Instituto de Física, Universidade Federal da Bahia, Campus de Ondina, Travessa Barão de Jeremoabo, s/n, Salvador, BA 40170-280, Brazil;3. Departamento de Oceanografia, Instituto de Geociências, Universidade Federal da Bahia, Campus de Ondina, Travessa Barão de Jeremoabo, s/n, Salvador, BA 40170-280, Brazil |
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| Abstract: | This work explores the effect of a cyclonic mesoscale feature of the Brazil Current (BC) moving northward off SE Brazil (20° S–23° S) in the Nutrients-Phytoplankton-Zooplankton (NPZ) dynamics. We employ the contour dynamics technique in a quasi-geostrophic, inviscid, 1½-layer model set as a meridional jet flowing southward along a rigid western boundary. This hydrodynamical model is coupled to a conventional NPZ model. We evaluate two distinct scenarios: (1) Plankton in a mixed layer (ML) with time-variable depth and no entrainment and; (2) Plankton in an ML held at a fixed depth, which allows entrainment. We perform simulations with different ML depths representing summer (42 m) and winter (86 m) for the region of interest. The presence of the western boundary allows the cyclonic ring to propagate northward due to image effect. The eddy motion produces upwelling (downwelling) in the leading (trailing) edge resulting in different responses in the two scenarios examined. In the variable ML depth simulations, Z is favored relative to P because there is no injection of N. On the other hand, in the fixed ML depth simulations, P is favored relative to Z due to dilution. All simulations show P enrichment within the eddy, but winter simulations show a greater response to the physical forcing. We conclude that the cyclonic eddy shed from BC provides favorable conditions for planktonic growth. Winter-like conditions seem to be more favorable than summer-like ones and, therefore, present more intense blooms associated with the ring. |
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| Keywords: | Brazil Current Contour dynamics Cyclonic meander Mesoscale process NPZ model Upper ocean |
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