4.5 Article

The roles of vertical shear and topography on the eddy formation near the site of origin of the Brazil Current

Journal

CONTINENTAL SHELF RESEARCH
Volume 70, Issue -, Pages 46-60

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.csr.2013.10.001

Keywords

Brazil Current; Mesoscale activity; Abrolhos bank; Numerical modeling

Categories

Funding

  1. CNPq
  2. CAPES
  3. CNPq's Millenium Initiative
  4. SMAST
  5. UMASSD

Ask authors/readers for more resources

The site of origin of the Brazil Current (BC) is currently one of the less explored aspects of regional circulation and mesoscale activity in the west side of the South Atlantic Subtropical gyre. The few studies that are available, based either on in situ data or on numerical modeling, seems to agree that the region is characterized by relatively weak baroclinic flow, with substantial mesoscale activity, which is quite different from other western boundary current systems (e.g. Florida Current, in the North Atlantic). We present numerical simulations that show that the main realistic mesoscale features in the eddy-rich vicinities of the BC site of origin can be successfully modeled through the dynamical interaction between parameterized versions of two opposing mean western boundary currents (BC and North Brazil Undercurrent NBUC) and local topography, with no influence of remote dynamics or atmospheric forcing. Large BC-related anticyclones observed in previous work were reproduced and recurrently formed during the model run. Two additional sensitivity experiments were performed. When NBUC is removed from the physical setting, the BC interaction with topography is not sufficient to generate eddies similar to observations. When an idealized flat-bottom and a physiographic configuration with no Abrolhos and Royal Charlotte Banks are considered, the BC-NBUC interaction is also not capable of developing realistic mesoscale structures. Our geophysical instability analyses suggest that BC-NBUC vertical shear is promoting baroclinic energy fluxes from the mean flow to the perturbations, resulting in eddy formation and growth in the region. (C) 2013 Elsevier Ltd. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Fisheries

Seasonal variability of ichthyoneuston assemblage on the continental shelf and slope of the Southwest Atlantic Ocean, Brazil (20°-23°S)

Ana Cristina Teixeira Bonecker, Mario Katsuragawa, Marcia Salustiano de Castro, Claudia Namiki, Maria de Lourdes Zani-Teixeira, Igor Uchoa Farias, Ilson Carlos Almeida da Silveira

JOURNAL OF APPLIED ICHTHYOLOGY (2019)

Article Geochemistry & Geophysics

NPZ response to eddy-induced upwelling in a Brazil Current ring: A theoretical approach

Filipe Pereira, Ilson C. A. da Silveira, Glenn R. Flierl, Amit Tandon

DYNAMICS OF ATMOSPHERES AND OCEANS (2019)

Article Oceanography

Dipole-induced Central Water extrusions south of Abrolhos Bank (Brazil, 20.5°S)

Wilton Z. Arruda, Ilson C. A. da Silveira

CONTINENTAL SHELF RESEARCH (2019)

Article Oceanography

On the Steadiness and Instability of the Intermediate Western Boundary Current between 24° and 18°S

Dante C. Napolitano, Ilson C. A. da Silveira, Cesar B. Rocha, Glenn R. Flierl, Paulo H. R. Calil, Renato P. Martins

JOURNAL OF PHYSICAL OCEANOGRAPHY (2019)

Article Oceanography

On the Role of Turbulent Mixing Produced by Vertical Shear Between the Brazil Current and the Intermediate Western Boundary Current

Caue Z. Lazaneo, Dante C. Napolitano, Ilson C. A. da Silveira, Amit Tandon, Daniel G. MacDonald, Rafael A. Avila, Paulo H. R. Calil

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2020)

Article Meteorology & Atmospheric Sciences

Development of a feature-oriented regional modelling system for the North Brazil Undercurrent region (1°-11°S) and its application to a process study on the genesis of the Potiguar Eddy

Ana Paula Morais Krelling, Avijit Gangopadhyay, Ilson da Silveira, Felipe Vilela-Silva

Summary: This study develops the key elements of a Feature-oriented regional modelling system in the Western Equatorial Atlantic, showing its potential applicability for operational forecasts and process studies. Through numerical experiments, it is found that the Potiguar Eddy can be generated by the North Brazil Undercurrent, with the induced vertical shear from the Deep Western Boundary Current affecting the eddy's characteristics.

JOURNAL OF OPERATIONAL OCEANOGRAPHY (2022)

Article Remote Sensing

Discrepancies between satellite-derived and in situ SST data in the Cape Frio Upwelling System, Southeastern Brazil (23&x2da;S)

F. Pereira, M. Bouali, P. S. Polito, I. C. A. da Silveira, R. N. Candella

REMOTE SENSING LETTERS (2020)

Article Oceanography

A Newly Observed Quasi-stationary Subsurface Anticyclone of the North Brazil Undercurrent at 4°S: The Potiguar Eddy

Ana P. M. Krelling, Ilson C. A. da Silveira, Paulo S. Polito, Avijit Gangopadhyay, Renato P. Martins, Jose Antonio M. Lima, Fernando de O. Marin

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2020)

Article Oceanography

Can the Intermediate Western Boundary Current recirculation trigger the Vitoria Eddy formation?

Dante C. Napolitano, Cesar B. Rocha, Ilson C. A. da Silveira, Iury T. Simoes-Sousa, Glenn R. Flierl

Summary: The Brazil Current meanders cyclonically within Tubarao Bight, occasionally forming the Vitoria Eddy, influenced by the Intermediate Western Boundary Current recirculating within the bight. A simple two-layer quasi-geostrophic model was used to study the effects of IWBC recirculation on BC meandering and Vitoria Eddy formation, showing that the strength of BC upstream of Tubarao Bight affects the formation of the eddy. The model experiments demonstrated that the interaction between the upper-layer jet and the lower-layer eddy plays a key role in triggering downstream meander growth and cyclone formation.

OCEAN DYNAMICS (2021)

Article Oceanography

Submesoscale Phenomena Due to the Brazil Current Crossing of the Vitoria-Trindade Ridge

D. C. Napolitano, I. C. A. da Silveira, A. Tandon, P. H. R. Calil

Summary: The Brazil Current and the Intermediate Western Boundary Current interact with the Vitoria-Trindade Ridge at 20.5 degrees S, generating mesoscale variability and unaddressed submesoscale dynamics. New observations and a high-resolution model are used to analyze the role of the VTR seamounts in the regional submesoscale dynamics, revealing submesoscale instabilities and flow-topography interactions. The lack of observations remains the main obstacle to better understand submesoscale processes in the oligotrophic South Atlantic where the VTR emerges as a submesoscale hotspot.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2021)

Article Oceanography

Revisiting the Atlantic South Equatorial Current

C. D. Luko, I. C. A. da Silveira, I. T. Simoes-Sousa, J. M. Araujo, A. Tandon

Summary: The southern branch of the South Equatorial Current is the northern limit of the South Atlantic Subtropical Gyre, bifurcating into the Brazil Current and North Brazil Undercurrent when it reaches Brazil. This study shows that the South Equatorial Current arrives at the South Atlantic western boundary as a multi-banded flow with different subsurface cores, influencing the seasonality of the Brazil Current and mesoscale eddies off Brazil.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2021)

Article Oceanography

Submesoscale Coherent Vortices in the South Atlantic Ocean: A Pathway for Energy Dissipation

C. Z. Lazaneo, P. H. R. Calil, A. Tandon, I. C. A. da Silveira

Summary: Mesoscale eddies in the South Atlantic propagate westward and interact with the Vitoria-Trindade Ridge, leading to the formation of submesoscale coherent vortices (SCVs). The dynamics of two adjacent SCVs wandering through the ridge are described using high-resolution measurements. It is found that the anticyclonic SCVs exhibit low potential vorticity and angular momentum, and are prone to small-scale turbulence and energy dissipation.

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS (2022)

Article Environmental Sciences

The Barreirinhas Eddies: Stable Energetic Anticyclones in the Near-Equatorial South Atlantic

Iury T. Simoes-Sousa, Ilson Carlos A. Silveira, Amit Tandon, Glenn R. Flierl, Cesar H. A. Ribeiro, Renato P. Martins

Summary: This study explores the Barreirinhas Eddies, submesoscale vortices generated by the North Brazil Current, which occur independently at different depths with incredibly high Rossby Numbers. Analysis suggests that the increased stability of these eddies is due to the joint effect of strong winds, stratification, proximity to the equator, and topography.

FRONTIERS IN MARINE SCIENCE (2021)

Article Environmental Sciences

Multidisciplinary Scientific Cruise to the Rio Grande Rise

Luigi Jovane, James R. Hein, Isobel A. Yeo, Mariana Benites, Natascha M. Bergo, Paulo V. F. Correa, Daniel M. Couto, Ayrton D. Guimaraes, Sarah A. Howarth, Henrique R. Miguel, Kira L. Mizell, Denise S. Moura, Francisco L. Vicentini Neto, Mayza Pompeu, Ianco M. M. Rodrigues, Frederico R. Santana, Pedro F. Serrao, Tomas E. Silva, Pedro M. Tura, Carolina L. Viscarra, Mateus G. Chuqui, Vivian H. Pellizari, Camila N. Signori, Ilson C. A. Da Silveira, Paulo Y. G. Sumida, Bramley J. Murton, Frederico P. Brandini

FRONTIERS IN MARINE SCIENCE (2019)

Article Physics, Fluids & Plasmas

Filaments, Fronts and Eddies in the Cabo Frio Coastal Upwelling System, Brazil

Paulo H. R. Calil, Nobuhiro Suzuki, Burkard Baschek, Ilson C. A. da Silveira

Summary: The study investigates the dynamics of meso- and submesoscale features in the northern South Brazil Bight shelf region using a regional model with 500-m horizontal resolution. Focus is on the Cabo Frio upwelling center, where nutrient-rich coastal waters are transported into the mid- and outer shelf, impacting local and remote productivity. During the upwelling phase, an intense front with strong horizontal temperature gradients and surface-intensified frontal jet develop, creating a preferential cross-shelf transport pathway.

FLUIDS (2021)

Article Oceanography

Temporal and spatial comparisons of ocean quahog (Arctica islandica) growth and lifespan on the mid-Atlantic continental shelf during inshore transgressions of their range from the Neoglacial through the twentieth century

Alyssa M. LeClaire, Eric N. Powell, Roger Mann, Kathleen M. Hemeon, Sara M. Pace, Vincent Saba, Hubert du Pontavice, Jillian R. Sower

Summary: Arctica islandica is an important species for recording climate change on the U.S. northeast continental shelf, and its growth rates show synchronous changes with cold and warm climatic periods. This study finds that A. islandica near the Delmarva Peninsula had higher growth rates during cold periods, possibly due to increased food supply in shallower water. The range recession of this species is a long-term process determined by the survivorship of older individuals.

CONTINENTAL SHELF RESEARCH (2024)