var bibbase_data = {"data":"<img src=\"//bibbase.org/img/ajax-loader.gif\" id=\"spinner\"\n  style=\"display: none;\" alt=\"Loading..\" />\n\n<div id=\"bibbase\">\n\n  <script type=\"text/javascript\">\n    var bibbase = {\n      params: {\"bib\":\"https://iuryt.github.io/pubs.bib\",\"jsonp\":\"1\",\"theme\":\"default\",\"host\":\"bibbase.org\"},\n      data: [{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"The Brazil Current quasi-stationary unstable meanders at 22°S–23°S\",\"journal\":\"Progress in Oceanography\",\"pages\":\"102925\",\"year\":\"2022\",\"issn\":\"0079-6611\",\"doi\":\"https://doi.org/10.1016/j.pocean.2022.102925\",\"url\":\"https://www.sciencedirect.com/science/article/pii/S0079661122001847\",\"author\":[{\"firstnames\":[\"Ilson\",\"C.A.\"],\"propositions\":[],\"lastnames\":[\"Silveira\"],\"suffixes\":[]},{\"firstnames\":[\"Filipe\"],\"propositions\":[],\"lastnames\":[\"Pereira\"],\"suffixes\":[]},{\"firstnames\":[\"Glenn\",\"R.\"],\"propositions\":[],\"lastnames\":[\"Flierl\"],\"suffixes\":[]},{\"firstnames\":[\"Iury\",\"T.\"],\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"suffixes\":[]},{\"firstnames\":[\"André\"],\"propositions\":[],\"lastnames\":[\"Palóczy\"],\"suffixes\":[]},{\"firstnames\":[\"Milton\"],\"propositions\":[],\"lastnames\":[\"Borges-Silva\"],\"suffixes\":[]},{\"firstnames\":[\"César\",\"B.\"],\"propositions\":[],\"lastnames\":[\"Rocha\"],\"suffixes\":[]}],\"keywords\":\"Brazil current, Baroclinic instability, Mesoscale eddies, Western boundary currents, Conservation of potential vorticity, Contour dynamics, South Atlantic, Cape Frio, Cape São Tomé\",\"abstract\":\"The most conspicuous oceanographic features off Southeastern Brazil are the quasi-stationary eddies formed off Capes São Tomé (CSTE) and Frio (CFE) associated with the Brazil Current (BC). We use SST and SSH products to infer eddy growth rates. These two independent data sets reveal an average growth rate of 0.06day-1, and propagation speeds are virtually null. CFE tends to be more unstable and frequent than CSTE (3.5 vs. 2.3 events per year). CSTE can propagate toward the north or south while CFE only propagates southward. We perform potential vorticity (PV) inversion calculation using hydrographic data to understand how the meander growth occurs in the baroclinic jet formed by the BC and the Intermediate Western Boundary Current (IWBC). PV anomalies in one layer enhanced the anomalies on the other. This result offered in situ evidence of baroclinic conversion occurring during the eddy event captured in the observations. We then build a theoretical two-layer model calibrated with the observations seeking to explain why the eddies grow in place, and no accompanying unstable anticyclones are formed. The experiments lead us to conclude that the eddies’ quasi-stationarity is due to the almost pure baroclinic nature of the BC-IWBC jet. We also find that the western boundary inhibits the formation of the anticyclones. As observed in satellite imagery, the meanders develop as isolated disturbances that may grow simultaneously or not.\",\"bibtex\":\"@article{silveira2022,\\ntitle = {The Brazil Current quasi-stationary unstable meanders at 22°S–23°S},\\njournal = {Progress in Oceanography},\\npages = {102925},\\nyear = {2022},\\nissn = {0079-6611},\\ndoi = {https://doi.org/10.1016/j.pocean.2022.102925},\\nurl = {https://www.sciencedirect.com/science/article/pii/S0079661122001847},\\nauthor = {Ilson C.A. {Silveira} and Filipe Pereira and Glenn R. Flierl and Iury T. Simoes-Sousa and André Palóczy and Milton Borges-Silva and César B. Rocha},\\nkeywords = {Brazil current, Baroclinic instability, Mesoscale eddies, Western boundary currents, Conservation of potential vorticity, Contour dynamics, South Atlantic, Cape Frio, Cape São Tomé},\\nabstract = {The most conspicuous oceanographic features off Southeastern Brazil are the quasi-stationary eddies formed off Capes São Tomé (CSTE) and Frio (CFE) associated with the Brazil Current (BC). We use SST and SSH products to infer eddy growth rates. These two independent data sets reveal an average growth rate of 0.06day-1, and propagation speeds are virtually null. CFE tends to be more unstable and frequent than CSTE (3.5 vs. 2.3 events per year). CSTE can propagate toward the north or south while CFE only propagates southward. We perform potential vorticity (PV) inversion calculation using hydrographic data to understand how the meander growth occurs in the baroclinic jet formed by the BC and the Intermediate Western Boundary Current (IWBC). PV anomalies in one layer enhanced the anomalies on the other. This result offered in situ evidence of baroclinic conversion occurring during the eddy event captured in the observations. We then build a theoretical two-layer model calibrated with the observations seeking to explain why the eddies grow in place, and no accompanying unstable anticyclones are formed. The experiments lead us to conclude that the eddies’ quasi-stationarity is due to the almost pure baroclinic nature of the BC-IWBC jet. We also find that the western boundary inhibits the formation of the anticyclones. As observed in satellite imagery, the meanders develop as isolated disturbances that may grow simultaneously or not.}\\n}\\n\",\"author_short\":[\"Silveira, I. C.\",\"Pereira, F.\",\"Flierl, G. R.\",\"Simoes-Sousa, I. T.\",\"Palóczy, A.\",\"Borges-Silva, M.\",\"Rocha, C. B.\"],\"key\":\"silveira2022\",\"id\":\"silveira2022\",\"bibbaseid\":\"silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://www.sciencedirect.com/science/article/pii/S0079661122001847\"},\"keyword\":[\"Brazil current\",\"Baroclinic instability\",\"Mesoscale eddies\",\"Western boundary currents\",\"Conservation of potential vorticity\",\"Contour dynamics\",\"South Atlantic\",\"Cape Frio\",\"Cape São Tomé\"],\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"The Brazil Current mesoscale eddies: Altimetry-based characterization and tracking\",\"journal\":\"Deep Sea Research Part I: Oceanographic Research Papers\",\"pages\":\"103947\",\"year\":\"2022\",\"issn\":\"0967-0637\",\"doi\":\"10.1016/j.dsr.2022.103947\",\"url\":\"https://www.sciencedirect.com/science/article/pii/S0967063722002606\",\"author\":[{\"firstnames\":[\"Igor\"],\"propositions\":[],\"lastnames\":[\"Uchoa\"],\"suffixes\":[]},{\"firstnames\":[\"Iury\",\"T.\"],\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"suffixes\":[]},{\"firstnames\":[\"Ilson\",\"C.A.\"],\"propositions\":[\"da Silveira\"],\"lastnames\":[],\"suffixes\":[]}],\"keywords\":\"Eddy detection algorithm, Western boundary current, Brazil Current, South Atlantic, Mesoscale eddies, Altimetry\",\"abstract\":\"The Brazil Current (BC) has been reported as eddy-dominated, with recurrent formation of eddies and meanders along the margin. In this study, we characterize the variability of mesoscale eddies associated with this western boundary current from its origin site to the southern end of the South Brazil Bight (∼15°S – ∼28°S). We apply an eddy detection method on a 27-year multi-satellite altimetry product. We offer a first quantitative estimate of the eddy dominance along the BC path. On average, there are no major differences in the eddy parameters between cyclones and anticyclones. However, north of the 20∘S, the eddies are larger and slower in swirling speed, whereas the opposite patterns occur with the eddies south of 20∘S. Although there is no notable seasonality in the eddy formation in general, there is a tendency to form cyclones in the vicinity of capes and bights of the southeastern Brazilian shelfbreak. In contrast, there is a scattered horizontal distribution of anticyclone formation for most of the BC domain throughout the seasons. The Vitória, Cape São Tomé and Cape Frio Eddies account for ∼30% of the total cyclones in the analysis. The Vitória Eddy (VE) tends to be more often generated in austral autumn, the season of lowest kinetic energy and volume transport of the BC. The Cape São Tomé Eddy (CSTE) and Cape Frio Eddy (CFE) are more energetic in the seasons of the BC’s highest volume transport (austral spring and summer). Despite most of the eddies being described as quasi-stationary in the current literature, our analysis of the eddy trajectories showed that the VE, CFE and CSTE can detach and migrate off of the mean BC axis. We estimate that ∼30% of the CFE events pinch off and migrate southwestward. The CSTE and CFE presented the highest growth rates (0.08 and 0.07 day−1 , respectively) of the recurrent eddies. These results provide a first robust characterization of the BC mesoscale eddies.\",\"bibtex\":\"@article{uchoa2022,\\ntitle = {The Brazil Current mesoscale eddies: Altimetry-based characterization and tracking},\\njournal = {Deep Sea Research Part I: Oceanographic Research Papers},\\npages = {103947},\\nyear = {2022},\\nissn = {0967-0637},\\ndoi = {10.1016/j.dsr.2022.103947},\\nurl = {https://www.sciencedirect.com/science/article/pii/S0967063722002606},\\nauthor = {Igor Uchoa and Iury T. Simoes-Sousa and Ilson C.A. {da Silveira}},\\nkeywords = {Eddy detection algorithm, Western boundary current, Brazil Current, South Atlantic, Mesoscale eddies, Altimetry},\\nabstract = {The Brazil Current (BC) has been reported as eddy-dominated, with recurrent formation of eddies and meanders along the margin. In this study, we characterize the variability of mesoscale eddies associated with this western boundary current from its origin site to the southern end of the South Brazil Bight (∼15°S – ∼28°S). We apply an eddy detection method on a 27-year multi-satellite altimetry product. We offer a first quantitative estimate of the eddy dominance along the BC path. On average, there are no major differences in the eddy parameters between cyclones and anticyclones. However, north of the 20∘S, the eddies are larger and slower in swirling speed, whereas the opposite patterns occur with the eddies south of 20∘S. Although there is no notable seasonality in the eddy formation in general, there is a tendency to form cyclones in the vicinity of capes and bights of the southeastern Brazilian shelfbreak. In contrast, there is a scattered horizontal distribution of anticyclone formation for most of the BC domain throughout the seasons. The Vitória, Cape São Tomé and Cape Frio Eddies account for ∼30% of the total cyclones in the analysis. The Vitória Eddy (VE) tends to be more often generated in austral autumn, the season of lowest kinetic energy and volume transport of the BC. The Cape São Tomé Eddy (CSTE) and Cape Frio Eddy (CFE) are more energetic in the seasons of the BC’s highest volume transport (austral spring and summer). Despite most of the eddies being described as quasi-stationary in the current literature, our analysis of the eddy trajectories showed that the VE, CFE and CSTE can detach and migrate off of the mean BC axis. We estimate that ∼30% of the CFE events pinch off and migrate southwestward. The CSTE and CFE presented the highest growth rates (0.08 and 0.07 day−1 , respectively) of the recurrent eddies. These results provide a first robust characterization of the BC mesoscale eddies.}\\n}\\n\",\"author_short\":[\"Uchoa, I.\",\"Simoes-Sousa, I. T.\",\"da Silveira , I. C.\"],\"key\":\"uchoa2022\",\"id\":\"uchoa2022\",\"bibbaseid\":\"uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://www.sciencedirect.com/science/article/pii/S0967063722002606\"},\"keyword\":[\"Eddy detection algorithm\",\"Western boundary current\",\"Brazil Current\",\"South Atlantic\",\"Mesoscale eddies\",\"Altimetry\"],\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"T.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tandon\"],\"firstnames\":[\"Amit\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pereira\"],\"firstnames\":[\"Filipe\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lazaneo\"],\"firstnames\":[\"Caue\",\"Z.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Mahadevan\"],\"firstnames\":[\"Amala\"],\"suffixes\":[]}],\"title\":\"Mixed layer eddies supply nutrients to enhance the spring phytoplankton bloom\",\"journal\":\"Frontiers in Marine Science\",\"volume\":\"9\",\"year\":\"2022\",\"url\":\"https://doi.org/10.3389/fmars.2022.825027\",\"doi\":\"10.3389/fmars.2022.825027\",\"issn\":\"2296-7745\",\"abstract\":\"Mixed layer eddies resulting from baroclinic instability of fronts convert horizontal buoyancy gradients into vertical stratification, shoaling the mixed layer. In light-limited regimes – high-latitudes – this process can initiate phytoplankton blooms prior to the springtime warming. The question is whether mixed layer eddies can enhance the spring bloom by delivering nutrients from beneath the mixed layer. We couple a submesoscale-resolving model (SUB) with a simple ecosystem model and examine the role of mixed layer eddies on the development of the spring bloom. We compare the SUB simulation to two coarser resolution (10 km) simulations, one that includes a mixed layer eddy parameterization (MLE) and another that prescribes the restratification from SUB and advects the biogeochemical tracers using geostrophic velocities (NVF). The MLE simulates restratification of the mixed layer and bloom onset, but the spring bloom has a deficit of 10–13% in the new production compared to SUB. The NVF has the same restratification as SUB, and with no vertical flux of nutrients, leads to a spring bloom with a 32–40% new production deficit compared to SUB. Submesoscale processes lead to exchange across the mixed layer base, which is not represented in coarse resolution model simulations, even with mixed layer eddy parameterizations. Our results show that nutrients supplied by mixed layer eddies are important to enhance the spring bloom.\",\"bibtex\":\"@ARTICLE{simoessousa2022b,\\nAUTHOR={Simoes-Sousa, Iury T. and Tandon, Amit and Pereira, Filipe and Lazaneo, Caue Z. and Mahadevan, Amala},   \\nTITLE={Mixed layer eddies supply nutrients to enhance the spring phytoplankton bloom},      \\nJOURNAL={Frontiers in Marine Science},      \\nVOLUME={9},           \\nYEAR={2022},        \\nURL={https://www.frontiersin.org/articles/10.3389/fmars.2022.825027},       \\nDOI={10.3389/fmars.2022.825027},\\nURL={https://doi.org/10.3389/fmars.2022.825027},\\nISSN={2296-7745},\\nabstract=\\\"Mixed layer eddies resulting from baroclinic instability of fronts convert horizontal buoyancy gradients into vertical stratification, shoaling the mixed layer. In light-limited regimes – high-latitudes – this process can initiate phytoplankton blooms prior to the springtime warming. The question is whether mixed layer eddies can enhance the spring bloom by delivering nutrients from beneath the mixed layer. We couple a submesoscale-resolving model (SUB) with a simple ecosystem model and examine the role of mixed layer eddies on the development of the spring bloom. We compare the SUB simulation to two coarser resolution (10 km) simulations, one that includes a mixed layer eddy parameterization (MLE) and another that prescribes the restratification from SUB and advects the biogeochemical tracers using geostrophic velocities (NVF). The MLE simulates restratification of the mixed layer and bloom onset, but the spring bloom has a deficit of 10–13% in the new production compared to SUB. The NVF has the same restratification as SUB, and with no vertical flux of nutrients, leads to a spring bloom with a 32–40% new production deficit compared to SUB. Submesoscale processes lead to exchange across the mixed layer base, which is not represented in coarse resolution model simulations, even with mixed layer eddy parameterizations. Our results show that nutrients supplied by mixed layer eddies are important to enhance the spring bloom.\\\",\\n}\\n\",\"author_short\":[\"Simoes-Sousa, I. T.\",\"Tandon, A.\",\"Pereira, F.\",\"Lazaneo, C. Z.\",\"Mahadevan, A.\"],\"key\":\"simoessousa2022b\",\"id\":\"simoessousa2022b\",\"bibbaseid\":\"simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.3389/fmars.2022.825027\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Atmospheric Cold Pools in the Bay of Bengal\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"T\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tandon\"],\"firstnames\":[\"Amit\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Buckley\"],\"firstnames\":[\"Jared\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Sengupta\"],\"firstnames\":[\"Debasis\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Shroyer\"],\"firstnames\":[\"Emily\"],\"suffixes\":[]},{\"propositions\":[\"de\"],\"lastnames\":[\"Szoeke\"],\"firstnames\":[\"Simon\",\"P\"],\"suffixes\":[]}],\"journal\":\"Journal of the Atmospheric Sciences\",\"doi\":\"10.1175/JAS-D-22-0041.1\",\"url\":\"https://doi.org/10.1175/JAS-D-22-0041.1\",\"year\":\"2022\",\"abstract\":\"Atmospheric cold pools, generated by evaporative downdrafts from precipitating clouds, are ubiquitous in the Bay of Bengal. We use data from three moorings near 18°N to characterize a total of 465 cold pools. The cold pools are all dry, with a typical temperature drop of 2°C (max. 5°C) and specific humidity drop of 1 g/kg (max. 6 g/kg). Most cold pools last 1.5-3.5 hours (max. 14 hours). Cold pools occur almost every day in the North Bay from April to November, principally in the late morning, associated with intense precipitation that accounts for 80% of total rain. They increase the latent heat flux to the atmosphere by about 32 W/m2(median), although the instantaneous enhancement of latent heat flux for individual cold pools reaches 150 W/m2 . During the rainiest month (July), the cold pools occur 21% of the time and contribute nearly 14% to the mean evaporation. A composite analysis of all cold pools shows that the temperature and specific humidity anomalies are responsible for  90% of the enhancement of sensible and latent heat flux, while variations in wind speed are responsible for the remainder. Depending on their gust front speed, the estimated height of the cold pools primarily ranges from 850 to 3200 m, with taller fronts more likely to occur during the summer monsoon season (Jun-Sep). Our results indicate that the realistic representation of cold pools in climate models is likely to be important for improved simulation of air-sea fluxes and monsoon rainfall.\",\"bibtex\":\"@article{simoessousa2022a,\\n  title={Atmospheric Cold Pools in the Bay of Bengal},\\n  author={Simoes-Sousa, Iury T and Tandon, Amit and Buckley, Jared and Sengupta, Debasis and Shroyer, Emily and de Szoeke, Simon P},\\n  journal={Journal of the Atmospheric Sciences},\\n  doi={10.1175/JAS-D-22-0041.1},\\n  url={https://doi.org/10.1175/JAS-D-22-0041.1},\\n  year={2022},\\n  abstract=\\\"Atmospheric cold pools, generated by evaporative downdrafts from precipitating clouds, are ubiquitous in the Bay of Bengal. We use data from three moorings near 18°N to characterize a total of 465 cold pools. The cold pools are all dry, with a typical temperature drop of 2°C (max. 5°C) and specific humidity drop of 1 g/kg (max. 6 g/kg). Most cold pools last 1.5-3.5 hours (max. 14 hours). Cold pools occur almost every day in the North Bay from April to November, principally in the late morning, associated with intense precipitation that accounts for 80% of total rain. They increase the latent heat flux to the atmosphere by about 32 W/m2(median), although the instantaneous enhancement of latent heat flux for individual cold pools reaches 150 W/m2 . During the rainiest month (July), the cold pools occur 21% of the time and contribute nearly 14% to the mean evaporation. A composite analysis of all cold pools shows that the temperature and specific humidity anomalies are responsible for ~90% of the enhancement of sensible and latent heat flux, while variations in wind speed are responsible for the remainder. Depending on their gust front speed, the estimated height of the cold pools primarily ranges from 850 to 3200 m, with taller fronts more likely to occur during the summer monsoon season (Jun-Sep). Our results indicate that the realistic representation of cold pools in climate models is likely to be important for improved simulation of air-sea fluxes and monsoon rainfall.\\\"\\n}\\n\",\"author_short\":[\"Simoes-Sousa, I. T\",\"Tandon, A.\",\"Buckley, J.\",\"Sengupta, D.\",\"Shroyer, E.\",\"de Szoeke, S. P\"],\"key\":\"simoessousa2022a\",\"id\":\"simoessousa2022a\",\"bibbaseid\":\"simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1175/JAS-D-22-0041.1\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Compact Mesoscale Eddies in the South Brazil Bight\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Rocha\"],\"firstnames\":[\"Cesar\",\"B\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"T\"],\"suffixes\":[]}],\"journal\":\"Remote Sensing\",\"volume\":\"14\",\"number\":\"22\",\"pages\":\"5781\",\"year\":\"2022\",\"publisher\":\"MDPI\",\"doi\":\"10.3390/rs14225781\",\"url\":\"https://doi.org/10.3390/rs14225781\",\"abstract\":\"Recent studies suggest that the South Brazil Bight (SBB) hosts strong westward propagating mesoscale eddies. We use 28 years of satellite altimetry data and a new Eddy Atlas to estimate how much of the eddy kinetic energy (EKE) observed in the SBB is accounted for by local eddies, generated in the Brazil Current (BC) region, versus remote eddies generated eastward of the BC region. First, we estimate a BC frontal density to obtain a robust definition of BC region. The BC front is well-defined throughout the SBB, occupying the region between the 200-m and 1000-m isobath, except in eddy hotspots downstream of sharp inflections of the continental slope, where the EKE far exceeds the mean kinetic energy (MKE). Compact, closed-contour mesoscale eddies account for 30–50% of the total EKE observed in the SBB, with local eddies accounting for most of the compact EKE in the BC region, defined as the area within 200 km of the 28-year mean BC front. Remote compact eddies account for less than 10% of the EKE observed in the BC region; compact eddies generated at long distances from the SBB, including eddies generated in the Southeastern Atlantic, contribute an insignificant fraction of EKE in the BC region.\",\"bibtex\":\"@article{rocha2022,\\n  title={Compact Mesoscale Eddies in the South Brazil Bight},\\n  author={Rocha, Cesar B and Simoes-Sousa, Iury T},\\n  journal={Remote Sensing},\\n  volume={14},\\n  number={22},\\n  pages={5781},\\n  year={2022},\\n  publisher={MDPI},\\n  doi={10.3390/rs14225781},\\n  url={https://doi.org/10.3390/rs14225781},\\n  abstract=\\\"Recent studies suggest that the South Brazil Bight (SBB) hosts strong westward propagating mesoscale eddies. We use 28 years of satellite altimetry data and a new Eddy Atlas to estimate how much of the eddy kinetic energy (EKE) observed in the SBB is accounted for by local eddies, generated in the Brazil Current (BC) region, versus remote eddies generated eastward of the BC region. First, we estimate a BC frontal density to obtain a robust definition of BC region. The BC front is well-defined throughout the SBB, occupying the region between the 200-m and 1000-m isobath, except in eddy hotspots downstream of sharp inflections of the continental slope, where the EKE far exceeds the mean kinetic energy (MKE). Compact, closed-contour mesoscale eddies account for 30–50% of the total EKE observed in the SBB, with local eddies accounting for most of the compact EKE in the BC region, defined as the area within 200 km of the 28-year mean BC front. Remote compact eddies account for less than 10% of the EKE observed in the BC region; compact eddies generated at long distances from the SBB, including eddies generated in the Southeastern Atlantic, contribute an insignificant fraction of EKE in the BC region.\\\",\\n}\\n\",\"author_short\":[\"Rocha, C. B\",\"Simoes-Sousa, I. T\"],\"key\":\"rocha2022\",\"id\":\"rocha2022\",\"bibbaseid\":\"rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.3390/rs14225781\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"The Barreirinhas Eddies: Stable energetic anticyclones in the near-equatorial South Atlantic\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"T\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Silveira\"],\"firstnames\":[\"Ilson\",\"Carlos\",\"A\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tandon\"],\"firstnames\":[\"Amit\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Flierl\"],\"firstnames\":[\"Glenn\",\"R\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Ribeiro\"],\"firstnames\":[\"Cesar\",\"HA\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Martins\"],\"firstnames\":[\"Renato\",\"P\"],\"suffixes\":[]}],\"journal\":\"Frontiers in Marine Science\",\"url\":\"https://doi.org/10.3389/fmars.2021.617011\",\"doi\":\"10.3389/fmars.2021.617011\",\"volume\":\"8\",\"pages\":\"28\",\"year\":\"2021\",\"publisher\":\"Frontiers\",\"abstract\":\"We explore the Barreirinhas Eddies, submesoscale vortices generated by the North Brazil Current (NBC) off the Barreirinhas Bight (Brazil, centered at 1.75°S), using vessel-mounted and moored ADCP data, and a Global HYCOM reanalysis. These double-stacked anticyclones with incredibly high Rossby Number [O(10)] occur independently at different depths (high Burger number). Anticyclones with Rossby number greater than unity are unstable according to inviscid linear theory, and hence these submesoscale features are not easily observable at mid latitudes. At these low latitudes, they last about a week, allowing characterization by oceanographic surveys. Our analyses suggest this increased stability is due to the joint effect of strong winds, stratification, proximity to the equator, and topography. Heretofore hypothesized via analytical studies and seen in numerical models, our study confirms this stabilization process in observations, and is also a starting point for the description of the submesoscale dynamics in the NBC domain.\",\"bibtex\":\"@article{simoes2021barreirinhas,\\n  title={The Barreirinhas Eddies: Stable energetic anticyclones in the near-equatorial South Atlantic},\\n  author={Simoes-Sousa, Iury T and Silveira, Ilson Carlos A and Tandon, Amit and Flierl, Glenn R and Ribeiro, Cesar HA and Martins, Renato P},\\n  journal={Frontiers in Marine Science},\\n  url = {https://doi.org/10.3389/fmars.2021.617011},\\n  doi = {10.3389/fmars.2021.617011},\\n  volume={8},\\n  pages={28},\\n  year={2021},\\n  publisher={Frontiers},\\n  abstract=\\\"We explore the Barreirinhas Eddies, submesoscale vortices generated by the North Brazil Current (NBC) off the Barreirinhas Bight (Brazil, centered at 1.75°S), using vessel-mounted and moored ADCP data, and a Global HYCOM reanalysis. These double-stacked anticyclones with incredibly high Rossby Number [O(10)] occur independently at different depths (high Burger number). Anticyclones with Rossby number greater than unity are unstable according to inviscid linear theory, and hence these submesoscale features are not easily observable at mid latitudes. At these low latitudes, they last about a week, allowing characterization by oceanographic surveys. Our analyses suggest this increased stability is due to the joint effect of strong winds, stratification, proximity to the equator, and topography. Heretofore hypothesized via analytical studies and seen in numerical models, our study confirms this stabilization process in observations, and is also a starting point for the description of the submesoscale dynamics in the NBC domain.\\\",\\n}\\n\",\"author_short\":[\"Simoes-Sousa, I. T\",\"Silveira, I. C. A\",\"Tandon, A.\",\"Flierl, G. R\",\"Ribeiro, C. H.\",\"Martins, R. P\"],\"key\":\"simoes2021barreirinhas\",\"id\":\"simoes2021barreirinhas\",\"bibbaseid\":\"simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.3389/fmars.2021.617011\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Can the Intermediate Western Boundary Current recirculation trigger the Vitória Eddy formation?\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Napolitano\"],\"firstnames\":[\"Dante\",\"C\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Rocha\"],\"firstnames\":[\"Cesar\",\"B\"],\"suffixes\":[]},{\"propositions\":[\"da\"],\"lastnames\":[\"Silveira\"],\"firstnames\":[\"Ilson\",\"CA\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"T\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Flierl\"],\"firstnames\":[\"Glenn\",\"R\"],\"suffixes\":[]}],\"journal\":\"Ocean Dynamics\",\"url\":\"https://doi.org/10.1007/s10236-020-01437-6\",\"doi\":\"10.1007/s10236-020-01437-6\",\"volume\":\"71\",\"number\":\"3\",\"pages\":\"281–292\",\"year\":\"2021\",\"publisher\":\"Springer Berlin Heidelberg\",\"abstract\":\"South of the Vitória-Trindade Ridge, a seamount chain off East Brazil, the Brazil Current (BC) meanders cyclonically within Tubarão Bight, occasionally forming the Vitória Eddy. It was recently found that the Intermediate Western Boundary Current (IWBC), which flows equatorward below the BC, cyclonically recirculate within Tubarão Bight. We present an analysis of AVISO observations that suggest that the Vitória Eddy formation is conditioned by the strength of the BC upstream of Tubarão Bight. A weak BC is prone to local meandering and eddy formation in the bight, while a strong BC suppresses eddy formation in the bight but triggers downstream meander growth. To study the effects of the IWBC recirculation on the BC meandering and the Vitória Eddy formation, we formulate a simple two-layer quasi-geostrophic model. In the model, the BC is represented by a meridional jet in the upper layer and the IWBC recirculation is a steady eddy in the lower layer. The lower-layer eddy effectively acts as a topographic bump, affecting the upper-layer jet via the stretching term \\\\(ψ _2/R_d^2\\\\), where ψ2 is the lower-layer streamfunction and Rd is the baroclinic deformation radius. Based on the AVISO sea-surface height data and previous observational studies, we define a stationary eddy and reference jet. We conduct a number of initial-value problem experiments varying the upper-layer jet speed. A weak upper-layer jet slowly meanders and develops a cyclone above the lower-layer eddy. As we increase the jet velocity, the meandering is faster and the cyclone is larger. But a too-strong jet has an opposite effect: the potential vorticity anomalies induced by the lower-layer eddy are quickly swept away, leading to explosive downstream meander growth; no cyclone is formed above the lower-layer eddy. In all cases, the initial meandering trigger is a linear process (the steering of the upper-layer jet by the lower-layer eddy). But even when the upper-layer jet is weak, nonlinearity quickly becomes important, dominating the dynamics after 10 days of simulation. The downstream meander growth is fully nonlinear. Our idealized QG model confirms that the IWBC recirculation can trigger the Vitória Eddy formation and elucidates the mechanisms involved in this process.\",\"bibtex\":\"@article{napolitano2021can,\\n  title={Can the Intermediate Western Boundary Current recirculation trigger the Vit{\\\\'o}ria Eddy formation?},\\n  author={Napolitano, Dante C and Rocha, Cesar B and da Silveira, Ilson CA and Simoes-Sousa, Iury T and Flierl, Glenn R},\\n  journal={Ocean Dynamics},\\n  url = {https://doi.org/10.1007/s10236-020-01437-6},\\n  doi = {10.1007/s10236-020-01437-6},\\n  volume={71},\\n  number={3},\\n  pages={281--292},\\n  year={2021},\\n  publisher={Springer Berlin Heidelberg},\\n  abstract=\\\"South of the Vitória-Trindade Ridge, a seamount chain off East Brazil, the Brazil Current (BC) meanders cyclonically within Tubarão Bight, occasionally forming the Vitória Eddy. It was recently found that the Intermediate Western Boundary Current (IWBC), which flows equatorward below the BC, cyclonically recirculate within Tubarão Bight. We present an analysis of AVISO observations that suggest that the Vitória Eddy formation is conditioned by the strength of the BC upstream of Tubarão Bight. A weak BC is prone to local meandering and eddy formation in the bight, while a strong BC suppresses eddy formation in the bight but triggers downstream meander growth. To study the effects of the IWBC recirculation on the BC meandering and the Vitória Eddy formation, we formulate a simple two-layer quasi-geostrophic model. In the model, the BC is represented by a meridional jet in the upper layer and the IWBC recirculation is a steady eddy in the lower layer. The lower-layer eddy effectively acts as a topographic bump, affecting the upper-layer jet via the stretching term \\\\(\\\\psi _{2}/{R_{d}^{2}}\\\\), where ψ2 is the lower-layer streamfunction and Rd is the baroclinic deformation radius. Based on the AVISO sea-surface height data and previous observational studies, we define a stationary eddy and reference jet. We conduct a number of initial-value problem experiments varying the upper-layer jet speed. A weak upper-layer jet slowly meanders and develops a cyclone above the lower-layer eddy. As we increase the jet velocity, the meandering is faster and the cyclone is larger. But a too-strong jet has an opposite effect: the potential vorticity anomalies induced by the lower-layer eddy are quickly swept away, leading to explosive downstream meander growth; no cyclone is formed above the lower-layer eddy. In all cases, the initial meandering trigger is a linear process (the steering of the upper-layer jet by the lower-layer eddy). But even when the upper-layer jet is weak, nonlinearity quickly becomes important, dominating the dynamics after 10 days of simulation. The downstream meander growth is fully nonlinear. Our idealized QG model confirms that the IWBC recirculation can trigger the Vitória Eddy formation and elucidates the mechanisms involved in this process.\\\",\\n}\\n\",\"author_short\":[\"Napolitano, D. C\",\"Rocha, C. B\",\"da Silveira, I. C.\",\"Simoes-Sousa, I. T\",\"Flierl, G. R\"],\"key\":\"napolitano2021can\",\"id\":\"napolitano2021can\",\"bibbaseid\":\"napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1007/s10236-020-01437-6\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Shroyer\"],\"firstnames\":[\"Emily\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tandon\"],\"firstnames\":[\"Amit\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Sengupta\"],\"firstnames\":[\"Debasis\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fernando\"],\"firstnames\":[\"Harindra\",\"JS\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lucas\"],\"firstnames\":[\"Andrew\",\"J\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Farrar\"],\"firstnames\":[\"J\",\"Thomas\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chattopadhyay\"],\"firstnames\":[\"Rajib\"],\"suffixes\":[]},{\"propositions\":[\"de\"],\"lastnames\":[\"Szoeke\"],\"firstnames\":[\"Simon\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Flatau\"],\"firstnames\":[\"Maria\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Rydbeck\"],\"firstnames\":[\"Adam\"],\"suffixes\":[]},{\"firstnames\":[],\"propositions\":[],\"lastnames\":[\"others\"],\"suffixes\":[]}],\"journal\":\"Bulletin of the American Meteorological Society\",\"url\":\"https://doi.org/10.1175/BAMS-D-20-0113.1\",\"doi\":\"10.1175/BAMS-D-20-0113.1\",\"pages\":\"1–44\",\"year\":\"2021\",\"abstract\":\"In the Bay of Bengal, the warm, dry boreal spring concludes with the onset of the summer monsoon and accompanying southwesterly winds, heavy rains, and variable air-sea fluxes. Here, we summarize the 2018 monsoon onset using observations collected through the multinational Monsoon Intraseasonal Oscillations in the Bay of Bengal (MISO-BoB) program between the US, India, and Sri Lanka. MISO-BoB aims to improve understanding of monsoon intraseasonal variability, and the 2018 field effort captured the coupled air-sea response during a transition from active-to-break conditions in the central BoB. The active phase of the  20-day research cruise was characterized by warm sea surface temperature (SST > 30°C), cold atmospheric outflows with intermittent heavy rainfall, and increasing winds (from 2 to 15 m s−1). Accumulated rainfall exceeded 200 mm with 90% of precipitation occurring during the first week. The following break period was both dry and clear, with persistent 10−12 m s−1 wind and evaporation of 0.2 mm h−1. The evolving environmental state included a deepening ocean mixed layer (from  20 to 50 m), cooling SST (by   1°C), and warming/drying of the lower to mid-troposphere. Local atmospheric development was consistent with phasing of the large-scale intraseasonal oscillation. The upper ocean stores significant heat in the BoB, enough to maintain SST above 29°C despite cooling by surface fluxes and ocean mixing. Comparison with reanalysis indicates biases in air-sea fluxes, which may be related to overly cool prescribed SST. Resolution of such biases offers a path toward improved forecasting of transition periods in the monsoon.\",\"bibtex\":\"@article{shroyer2021bay,\\n  title={Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset},\\n  author={Shroyer, Emily and Tandon, Amit and Sengupta, Debasis and Fernando, Harindra JS and Lucas, Andrew J and Farrar, J Thomas and Chattopadhyay, Rajib and de Szoeke, Simon and Flatau, Maria and Rydbeck, Adam and others},\\n  journal={Bulletin of the American Meteorological Society},\\n  url = {https://doi.org/10.1175/BAMS-D-20-0113.1},\\n  doi = {10.1175/BAMS-D-20-0113.1},\\n  pages={1--44},\\n  year={2021},\\n  abstract=\\\"In the Bay of Bengal, the warm, dry boreal spring concludes with the onset of the summer monsoon and accompanying southwesterly winds, heavy rains, and variable air-sea fluxes. Here, we summarize the 2018 monsoon onset using observations collected through the multinational Monsoon Intraseasonal Oscillations in the Bay of Bengal (MISO-BoB) program between the US, India, and Sri Lanka. MISO-BoB aims to improve understanding of monsoon intraseasonal variability, and the 2018 field effort captured the coupled air-sea response during a transition from active-to-break conditions in the central BoB. The active phase of the ~20-day research cruise was characterized by warm sea surface temperature (SST > 30°C), cold atmospheric outflows with intermittent heavy rainfall, and increasing winds (from 2 to 15 m s−1). Accumulated rainfall exceeded 200 mm with 90\\\\% of precipitation occurring during the first week. The following break period was both dry and clear, with persistent 10−12 m s−1 wind and evaporation of 0.2 mm h−1. The evolving environmental state included a deepening ocean mixed layer (from ~20 to 50 m), cooling SST (by ~ 1°C), and warming/drying of the lower to mid-troposphere. Local atmospheric development was consistent with phasing of the large-scale intraseasonal oscillation. The upper ocean stores significant heat in the BoB, enough to maintain SST above 29°C despite cooling by surface fluxes and ocean mixing. Comparison with reanalysis indicates biases in air-sea fluxes, which may be related to overly cool prescribed SST. Resolution of such biases offers a path toward improved forecasting of transition periods in the monsoon.\\\",\\n}\\n\",\"author_short\":[\"Shroyer, E.\",\"Tandon, A.\",\"Sengupta, D.\",\"Fernando, H. J.\",\"Lucas, A. J\",\"Farrar, J T.\",\"Chattopadhyay, R.\",\"de Szoeke, S.\",\"Flatau, M.\",\"Rydbeck, A.\",\"others\"],\"key\":\"shroyer2021bay\",\"id\":\"shroyer2021bay\",\"bibbaseid\":\"shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1175/BAMS-D-20-0113.1\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Revisiting the Atlantic South Equatorial Current\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Luko\"],\"firstnames\":[\"CD\"],\"suffixes\":[]},{\"propositions\":[\"da\"],\"lastnames\":[\"Silveira\"],\"firstnames\":[\"ICA\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"IT\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Araujo\"],\"firstnames\":[\"JM\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tandon\"],\"firstnames\":[\"A\"],\"suffixes\":[]}],\"journal\":\"Journal of Geophysical Research: Oceans\",\"pages\":\"e2021JC017387\",\"url\":\"https://doi.org/10.1029/2021JC017387\",\"doi\":\"10.1029/2021JC017387\",\"year\":\"2021\",\"abstract\":\"The southern branch of the South Equatorial Current (SSEC) is the northern limit of the South Atlantic Subtropical Gyre. When this current reaches Brazil around 14°S it bifurcates into a southward flow as the Brazil Current (BC) and the surface portion of the northward flowing North Brazil Undercurrent (NBUC). The SSEC system is a key component of the western boundary supply, influencing the NBUC/BC variability and, therefore, global climate through the Meridional Overturning Circulation. In this study, using altimetry satellite data and reanalyzes outputs (1993–2018), we revisit the SSEC mean state and show this current arriving at the South Atlantic western boundary as a multi-banded flow with surface signatures resulting from different subsurface cores. These bands have velocities between 0.02 and 0.07 m s$^{−1}$ and, as shown by ADCP data from the PIRATA project, their signature in synoptic scenarios is obscured by eddies and waves with velocities between 0.1 and 0.3 m s$^{−1}$. In addition, the SSEC annual cycle analysis shows that the seasonality of the bands is out of phase with each other, presenting westward transport anomalies between 0.4 and 2.6 Sv. Finally, our results show that the seasonality of this multi-banded flow both defines where the BC is born, and modulates the seasonality of semi-permanent mesoscale eddies off Brazil.\",\"bibtex\":\"@article{luko2021revisiting,\\n  title={Revisiting the Atlantic South Equatorial Current},\\n  author={Luko, CD and da Silveira, ICA and Simoes-Sousa, IT and Araujo, JM and Tandon, A},\\n  journal={Journal of Geophysical Research: Oceans},\\n  pages={e2021JC017387},\\n  url = {https://doi.org/10.1029/2021JC017387},\\n  doi = {10.1029/2021JC017387},\\n  year={2021},\\n  abstract=\\\"The southern branch of the South Equatorial Current (SSEC) is the northern limit of the South Atlantic Subtropical Gyre. When this current reaches Brazil around 14°S it bifurcates into a southward flow as the Brazil Current (BC) and the surface portion of the northward flowing North Brazil Undercurrent (NBUC). The SSEC system is a key component of the western boundary supply, influencing the NBUC/BC variability and, therefore, global climate through the Meridional Overturning Circulation. In this study, using altimetry satellite data and reanalyzes outputs (1993–2018), we revisit the SSEC mean state and show this current arriving at the South Atlantic western boundary as a multi-banded flow with surface signatures resulting from different subsurface cores. These bands have velocities between 0.02 and 0.07 m s$^{−1}$ and, as shown by ADCP data from the PIRATA project, their signature in synoptic scenarios is obscured by eddies and waves with velocities between 0.1 and 0.3 m s$^{−1}$. In addition, the SSEC annual cycle analysis shows that the seasonality of the bands is out of phase with each other, presenting westward transport anomalies between 0.4 and 2.6 Sv. Finally, our results show that the seasonality of this multi-banded flow both defines where the BC is born, and modulates the seasonality of semi-permanent mesoscale eddies off Brazil.\\\",\\n}\\n\",\"author_short\":[\"Luko, C.\",\"da Silveira, I.\",\"Simoes-Sousa, I.\",\"Araujo, J.\",\"Tandon, A\"],\"key\":\"luko2021revisiting\",\"id\":\"luko2021revisiting\",\"bibbaseid\":\"luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1029/2021JC017387\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Insights on the non-linear solution of Munk's ocean circulation theory from a rotating tank experiment\",\"author\":[{\"firstnames\":[\"Paulo\",\"S.\"],\"propositions\":[],\"lastnames\":[\"Polito\"],\"suffixes\":[]},{\"firstnames\":[\"Olga\",\"T.\"],\"propositions\":[],\"lastnames\":[\"Sato\"],\"suffixes\":[]},{\"firstnames\":[\"Dante\",\"C.\"],\"propositions\":[],\"lastnames\":[\"Napolitano\"],\"suffixes\":[]},{\"firstnames\":[\"Iury\",\"T.\"],\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"suffixes\":[]},{\"firstnames\":[\"Helio\"],\"propositions\":[],\"lastnames\":[\"Almeida\"],\"suffixes\":[]},{\"firstnames\":[\"Fabricio\",\"R.\"],\"propositions\":[],\"lastnames\":[\"Lapolli\"],\"suffixes\":[]}],\"journal\":\"Ocean and Coastal Research\",\"doi\":\"10.1590/2675-2824069.20-011psp\",\"url\":\"https://doi.org/10.1590/2675-2824069.20-011psp\",\"year\":\"2021\",\"publisher\":\"FapUNIFESP (SciELO)\",\"volume\":\"69\",\"abstract\":\"At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk's circulation theory aided by a Lagrangian particles tracking algorithm and numerical modeling. From information captured by video, we track the trajectories of drifters, and then objectively mapped the streamfunction to obtain the mean circulation pattern. We were able to reproduce the wind-forced anticyclonic and asymmetric gyre, including the western boundary intensification and its retroflection. The latter phenomenon was predicted by the non-linear version of Munk's model and observed in real subtropical gyres as small recirculation regions. We have configured two numerical model simulations mimicking the physical experiment, with linear and non-linear terms. The comparison between the numerical and physical experiments confirmed the effect of non-linear distortion of the gyre. Geophysical fluid dynamics is often hard to visualize, and counter-intuitive in a rotating system. We present this set of experiments as a tool for oceanography teaching. Besides studying general ocean circulation theories and observations through practical examples, this experiment provides an opportunity to develop basic image processing and geophysical modelling skills.\",\"bibtex\":\"@article{polito2021,\\n  title = {Insights on the non-linear solution of Munk's ocean circulation theory from a rotating tank experiment},\\n  author = {Paulo S. Polito and Olga T. Sato and Dante C. Napolitano and Iury T. Simoes-Sousa and Helio Almeida and Fabricio R. Lapolli},\\n  journal = {Ocean and Coastal Research},\\n  doi = {10.1590/2675-2824069.20-011psp},\\n  url = {https://doi.org/10.1590/2675-2824069.20-011psp},\\n  year = {2021},\\n  publisher = {{FapUNIFESP} ({SciELO})},\\n  volume = {69},\\n  abstract = \\\"At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk's circulation theory aided by a Lagrangian particles tracking algorithm and numerical modeling. From information captured by video, we track the trajectories of drifters, and then objectively mapped the streamfunction to obtain the mean circulation pattern. We were able to reproduce the wind-forced anticyclonic and asymmetric gyre, including the western boundary intensification and its retroflection. The latter phenomenon was predicted by the non-linear version of Munk's model and observed in real subtropical gyres as small recirculation regions. We have configured two numerical model simulations mimicking the physical experiment, with linear and non-linear terms. The comparison between the numerical and physical experiments confirmed the effect of non-linear distortion of the gyre. Geophysical fluid dynamics is often hard to visualize, and counter-intuitive in a rotating system. We present this set of experiments as a tool for oceanography teaching. Besides studying general ocean circulation theories and observations through practical examples, this experiment provides an opportunity to develop basic image processing and geophysical modelling skills.\\\",\\n}\\n\",\"author_short\":[\"Polito, P. S.\",\"Sato, O. T.\",\"Napolitano, D. C.\",\"Simoes-Sousa, I. T.\",\"Almeida, H.\",\"Lapolli, F. R.\"],\"key\":\"polito2021\",\"id\":\"polito2021\",\"bibbaseid\":\"polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1590/2675-2824069.20-011psp\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Biological and Toxicological Evaluation of N-(4methyl-phenyl)-4-methylphthalimide on Bone Cancer in Mice\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Santin\"],\"firstnames\":[\"Jose\",\"R\"],\"suffixes\":[]},{\"propositions\":[\"da\"],\"lastnames\":[\"Silva\"],\"firstnames\":[\"Gislaine\",\"F\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pastor\"],\"firstnames\":[\"Maria\",\"VD\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Broering\"],\"firstnames\":[\"Milena\",\"F\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nunes\"],\"firstnames\":[\"Roberta\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Braga\"],\"firstnames\":[\"Rodolpho\",\"C\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"T.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Stiz\"],\"firstnames\":[\"Dorimar\",\"S\"],\"suffixes\":[]},{\"propositions\":[\"da\"],\"lastnames\":[\"Silva\"],\"firstnames\":[\"Kathryn\",\"ABS\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Stoeberl\"],\"firstnames\":[\"Luis\",\"C\"],\"suffixes\":[]},{\"firstnames\":[],\"propositions\":[],\"lastnames\":[\"others\"],\"suffixes\":[]}],\"journal\":\"Anti-Cancer Agents in Medicinal Chemistry (Formerly Current Medicinal Chemistry-Anti-Cancer Agents)\",\"url\":\"https://doi.org/10.2174/1871520619666190207130732\",\"doi\":\"10.2174/1871520619666190207130732\",\"volume\":\"19\",\"number\":\"5\",\"pages\":\"667–676\",\"year\":\"2019\",\"publisher\":\"Bentham Science Publishers\",\"bibtex\":\"@article{santin2019biological,\\n  title={Biological and Toxicological Evaluation of N-(4methyl-phenyl)-4-methylphthalimide on Bone Cancer in Mice},\\n  author={Santin, Jose R and da Silva, Gislaine F and Pastor, Maria VD and Broering, Milena F and Nunes, Roberta and Braga, Rodolpho C and Simoes-Sousa, Iury T. and Stiz, Dorimar S and da Silva, Kathryn ABS and Stoeberl, Luis C and others},\\n  journal={Anti-Cancer Agents in Medicinal Chemistry (Formerly Current Medicinal Chemistry-Anti-Cancer Agents)},\\n  url = {https://doi.org/10.2174/1871520619666190207130732},\\n  doi = {10.2174/1871520619666190207130732},\\n  volume={19},\\n  number={5},\\n  pages={667--676},\\n  year={2019},\\n  publisher={Bentham Science Publishers}\\n}\\n\",\"author_short\":[\"Santin, J. R\",\"da Silva, G. F\",\"Pastor, M. V.\",\"Broering, M. F\",\"Nunes, R.\",\"Braga, R. C\",\"Simoes-Sousa, I. T.\",\"Stiz, D. S\",\"da Silva, K. A.\",\"Stoeberl, L. C\",\"others\"],\"key\":\"santin2019biological\",\"id\":\"santin2019biological\",\"bibbaseid\":\"santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.2174/1871520619666190207130732\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"As Correntes Oceânicas na Bacia Sergipe-Alagoas\",\"author\":[{\"firstnames\":[\"Ilson\"],\"propositions\":[],\"lastnames\":[\"Silveira\"],\"suffixes\":[]},{\"firstnames\":[\"Dante\"],\"propositions\":[],\"lastnames\":[\"Napolitano\"],\"suffixes\":[]},{\"firstnames\":[\"Iury\"],\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"suffixes\":[]},{\"firstnames\":[\"Renato\"],\"propositions\":[],\"lastnames\":[\"Parkinson\"],\"suffixes\":[]},{\"firstnames\":[\"Wandrey\"],\"propositions\":[],\"lastnames\":[\"Watanabe\"],\"suffixes\":[]}],\"journal\":\"Revista Marseal: Edição Águas Profundas SE/AL\",\"year\":\"2018\",\"volume\":\"2\",\"pages\":\"36–39\",\"issn\":\"2596-0547\",\"publisher\":\"Editora UFS e Centro de Pesquisas da Petrobras (CENPES)\",\"url\":\"https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/\",\"bibtex\":\"@article{marseal2018,\\n  title = {As Correntes Oceânicas na {Bacia Sergipe-Alagoas}},\\n  author = {Ilson Silveira and Dante Napolitano and Iury Simoes-Sousa and Renato Parkinson and Wandrey Watanabe},\\n  journal = {Revista Marseal: Edição Águas Profundas SE/AL},\\n  year = {2018},\\n  volume = {2},\\n  pages = {36--39},\\n  issn = {2596-0547},\\n  publisher = {Editora UFS e Centro de Pesquisas da Petrobras (CENPES)},\\n  url = {https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/}\\n}\\n\",\"author_short\":[\"Silveira, I.\",\"Napolitano, D.\",\"Simoes-Sousa, I.\",\"Parkinson, R.\",\"Watanabe, W.\"],\"key\":\"marseal2018\",\"id\":\"marseal2018\",\"bibbaseid\":\"silveira-napolitano-simoessousa-parkinson-watanabe-ascorrentesocenicasnabaciasergipealagoas-2018\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/\"},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Surfing the currents: The longest distance traveled by a released West Indian manatee (<i>Trichechus manatus</i>) and the implications for conservation\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Carvalho\"],\"firstnames\":[\"Camila\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Simoes-Sousa\"],\"firstnames\":[\"Iury\",\"Tercio\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Santos\"],\"firstnames\":[\"Lucas\",\"Pereira\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Choi-Lima\"],\"firstnames\":[\"Katherine\",\"Fiedler\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pereira\"],\"firstnames\":[\"Letícia\",\"Gonçalves\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Alves\"],\"firstnames\":[\"Maria\",\"Danise\",\"de\",\"Oliveira\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Carrero\"],\"firstnames\":[\"Adrian\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Santander\"],\"firstnames\":[\"Juan\",\"Carlos\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Carvalho\"],\"firstnames\":[\"Vitor\",\"Luz\"],\"suffixes\":[]}],\"journal\":\"Journal of the Marine Biological Association of the United Kingdom\",\"year\":\"2023\",\"note\":\"Under review.\",\"issn\":\"1469-7769\",\"bibtex\":\"@article{carvalho2023,\\n  title = {Surfing the currents: {T}he longest distance traveled by a released {W}est {I}ndian manatee (\\\\textit{{T}richechus manatus}) and the implications for conservation},\\n  author = {Carvalho, Camila and Simoes-Sousa, Iury Tercio and Santos, Lucas Pereira and Choi-Lima, Katherine Fiedler and Pereira, Letícia Gonçalves and Alves, Maria Danise de Oliveira and Carrero, Adrian and Santander, Juan Carlos and Carvalho, Vitor Luz},\\n  journal = {Journal of the Marine Biological Association of the United Kingdom},\\n  year = {2023},\\n  note = {Under review.},\\n  issn = {1469-7769}\\n}\\n\",\"author_short\":[\"Carvalho, C.\",\"Simoes-Sousa, I. T.\",\"Santos, L. P.\",\"Choi-Lima, K. F.\",\"Pereira, L. G.\",\"Alves, M. D. d. O.\",\"Carrero, A.\",\"Santander, J. C.\",\"Carvalho, V. L.\"],\"key\":\"carvalho2023\",\"id\":\"carvalho2023\",\"bibbaseid\":\"carvalho-simoessousa-santos-choilima-pereira-alves-carrero-santander-etal-surfingthecurrentsthelongestdistancetraveledbyareleasedwestindianmanateeitrichechusmanatusiandtheimplicationsforconservation-2023\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\"html\":\"\"}],\n      metadata: {\"owner\":\"simoes-sousa, i\",\"authorlinks\":{\"simoes-sousa, i\":\"https://iuryt.github.io/publications.html\"}},\n      ownerID: \"eBTKe5N5TDhwsAEsZ\"\n    };\n  </script>\n\n  <script type=\"text/javascript\">\n  var site$;\n  if (typeof $ != 'undefined') {\n    console.log('existing jquery: storing and then restoring');\n    site$ = $;\n    $ = null;\n  }\n  </script>\n\n  <script src=\"https://ajax.googleapis.com/ajax/libs/jquery/2.2.4/jquery.min.js\">\n  </script>\n  <script type=\"text/javascript\">\n  if (site$) {\n    console.log('existing jquery: avoiding conflict and restoring');\n    bb$ = $.noConflict(true);\n    $ = site$;\n  } else {\n    bb$ = $;\n  }\n  </script>\n\n  <script src=\"//bibbase.org/js/bibbase.min.js\"\n          type=\"text/javascript\">\n  </script>\n\n  <script type=\"text/javascript\"\n          src=\"https://cdnjs.cloudflare.com/ajax/libs/mathjax/2.7.1/MathJax.js?config=TeX-AMS-MML_HTMLorMML\">\n  </script>\n  <script type=\"text/x-mathjax-config\">\n    MathJax.Hub.Config({tex2jax: {inlineMath: [['$','$'], ['\\\\(','\\\\)']]},\n                        skipTags: [\"body\"],\n                        processClass: \"bibbase_paper\"});\n  </script>\n\n  <style>\n  @media print {\n    .dontprint {\n        display: none !important;\n    }\n\n  .bibbase_group {\n    background-color: #E0E0E0;\n    font-style: italic;\n    font-size: larger;\n    text-shadow: 0px 0px 3px #FFFFFF;\n    border-radius: 4px 4px 4px 4px;\n    -moz-border-radius: 4px 4px 4px 4px;\n    -webkit-border-radius: 4px;\n    padding: 5px 40px 5px;\n    margin-top: 10px;\n    margin-bottom: 5px;\n    cursor: pointer;\n  }\n\n  .bibbase_paper {\n    margin-bottom: 5px;\n  }\n\n  }\n  </style>\n\n  \n  <div style=\"float: right; margin-right: 10px; margin-top: 10px; text-align: right; font-size: 12px\">\n    generated by\n    <a href=\"//bibbase.org\"\n       onclick=\"trackOutboundLink('bibbase', 'logo clicked', window.location.href, '//bibbase.org'); return false;\">\n      <img src=\"//bibbase.org/img/logo.svg\"\n           style=\"vertical-align: middle; margin-left: 3px; height: 16px;\"/\n           alt=\"bibbase.org\"\n           title=\"BibBase – The easiest way to maintain your publications page.\"\n        ></a>\n    \n  </div>\n  \n\n  <div id=\"bibbase_header\" class=\"dontprint\" style=\"\">\n\n    <ul class=\"nav nav-pills\" style=\"margin: 0px;\">\n\n      <li class=\"dropdown\" id=\"groupby_dropdown\">\n      <a class=\"dropdown-toggle\"\n         data-toggle=\"dropdown\"\n         href=\"#\">\n          Group by\n          <b class=\"caret\"></b>\n      </a>\n      <ul class=\"dropdown-menu\">\n        <li class=\"groupby year\"><a onclick=\"groupby('year')\">\n            Year</a>\n        </li>\n        <li class=\"groupby author\"><a onclick=\"groupby('author_short')\">\n            Author</a>\n        </li>\n        <li class=\"groupby type\"><a onclick=\"groupby('type')\">\n            Type</a>\n        </li>\n        <li class=\"groupby keyword\"><a onclick=\"groupby('keyword')\">\n            Keyword</a>\n        </li>\n        <li class=\"groupby downloads\"><a onclick=\"groupby('downloads')\">\n            Downloads</a>\n        </li>\n      </ul>\n      </li>\n\n\n      <li class=\"dropdown\" id=\"menu_dropdown\">\n      <a class=\"dropdown-toggle\"\n         data-toggle=\"dropdown\"\n         href=\"#\" alt=\"controls\">\n          <i class=\"fa fa-reorder\" alt=\"controls\"></i>\n          <b class=\"caret\"></b>\n      </a>\n      <ul class=\"dropdown-menu\">\n        <li>\n          <a onclick=\"toggleAll()\">\n            <i class=\"fa fa-chevron-down fa-fw\"></i> Expand/Collapse All\n          </a>\n        </li>\n        <li>\n          <a download=\"pubs.bib\" href=\"data:text/bibtex;base64,@article{silveira2022,
title = {The Brazil Current quasi-stationary unstable meanders at 22°S–23°S},
journal = {Progress in Oceanography},
pages = {102925},
year = {2022},
issn = {0079-6611},
doi = {https://doi.org/10.1016/j.pocean.2022.102925},
url = {https://www.sciencedirect.com/science/article/pii/S0079661122001847},
author = {Ilson C.A. {Silveira} and Filipe Pereira and Glenn R. Flierl and Iury T. Simoes-Sousa and André Palóczy and Milton Borges-Silva and César B. Rocha},
keywords = {Brazil current, Baroclinic instability, Mesoscale eddies, Western boundary currents, Conservation of potential vorticity, Contour dynamics, South Atlantic, Cape Frio, Cape São Tomé},
abstract = {The most conspicuous oceanographic features off Southeastern Brazil are the quasi-stationary eddies formed off Capes São Tomé (CSTE) and Frio (CFE) associated with the Brazil Current (BC). We use SST and SSH products to infer eddy growth rates. These two independent data sets reveal an average growth rate of 0.06day-1, and propagation speeds are virtually null. CFE tends to be more unstable and frequent than CSTE (3.5 vs. 2.3 events per year). CSTE can propagate toward the north or south while CFE only propagates southward. We perform potential vorticity (PV) inversion calculation using hydrographic data to understand how the meander growth occurs in the baroclinic jet formed by the BC and the Intermediate Western Boundary Current (IWBC). PV anomalies in one layer enhanced the anomalies on the other. This result offered in situ evidence of baroclinic conversion occurring during the eddy event captured in the observations. We then build a theoretical two-layer model calibrated with the observations seeking to explain why the eddies grow in place, and no accompanying unstable anticyclones are formed. The experiments lead us to conclude that the eddies’ quasi-stationarity is due to the almost pure baroclinic nature of the BC-IWBC jet. We also find that the western boundary inhibits the formation of the anticyclones. As observed in satellite imagery, the meanders develop as isolated disturbances that may grow simultaneously or not.}
}


@article{uchoa2022,
title = {The Brazil Current mesoscale eddies: Altimetry-based characterization and tracking},
journal = {Deep Sea Research Part I: Oceanographic Research Papers},
pages = {103947},
year = {2022},
issn = {0967-0637},
doi = {10.1016/j.dsr.2022.103947},
url = {https://www.sciencedirect.com/science/article/pii/S0967063722002606},
author = {Igor Uchoa and Iury T. Simoes-Sousa and Ilson C.A. {da Silveira}},
keywords = {Eddy detection algorithm, Western boundary current, Brazil Current, South Atlantic, Mesoscale eddies, Altimetry},
abstract = {The Brazil Current (BC) has been reported as eddy-dominated, with recurrent formation of eddies and meanders along the margin. In this study, we characterize the variability of mesoscale eddies associated with this western boundary current from its origin site to the southern end of the South Brazil Bight (∼15°S – ∼28°S). We apply an eddy detection method on a 27-year multi-satellite altimetry product. We offer a first quantitative estimate of the eddy dominance along the BC path. On average, there are no major differences in the eddy parameters between cyclones and anticyclones. However, north of the 20∘S, the eddies are larger and slower in swirling speed, whereas the opposite patterns occur with the eddies south of 20∘S. Although there is no notable seasonality in the eddy formation in general, there is a tendency to form cyclones in the vicinity of capes and bights of the southeastern Brazilian shelfbreak. In contrast, there is a scattered horizontal distribution of anticyclone formation for most of the BC domain throughout the seasons. The Vitória, Cape São Tomé and Cape Frio Eddies account for ∼30% of the total cyclones in the analysis. The Vitória Eddy (VE) tends to be more often generated in austral autumn, the season of lowest kinetic energy and volume transport of the BC. The Cape São Tomé Eddy (CSTE) and Cape Frio Eddy (CFE) are more energetic in the seasons of the BC’s highest volume transport (austral spring and summer). Despite most of the eddies being described as quasi-stationary in the current literature, our analysis of the eddy trajectories showed that the VE, CFE and CSTE can detach and migrate off of the mean BC axis. We estimate that ∼30% of the CFE events pinch off and migrate southwestward. The CSTE and CFE presented the highest growth rates (0.08 and 0.07 day−1 , respectively) of the recurrent eddies. These results provide a first robust characterization of the BC mesoscale eddies.}
}


@ARTICLE{simoessousa2022b,
AUTHOR={Simoes-Sousa, Iury T. and Tandon, Amit and Pereira, Filipe and Lazaneo, Caue Z. and Mahadevan, Amala},   
TITLE={Mixed layer eddies supply nutrients to enhance the spring phytoplankton bloom},      
JOURNAL={Frontiers in Marine Science},      
VOLUME={9},           
YEAR={2022},        
URL={https://www.frontiersin.org/articles/10.3389/fmars.2022.825027},       
DOI={10.3389/fmars.2022.825027},
URL={https://doi.org/10.3389/fmars.2022.825027},
ISSN={2296-7745},
abstract="Mixed layer eddies resulting from baroclinic instability of fronts convert horizontal buoyancy gradients into vertical stratification, shoaling the mixed layer. In light-limited regimes – high-latitudes – this process can initiate phytoplankton blooms prior to the springtime warming. The question is whether mixed layer eddies can enhance the spring bloom by delivering nutrients from beneath the mixed layer. We couple a submesoscale-resolving model (SUB) with a simple ecosystem model and examine the role of mixed layer eddies on the development of the spring bloom. We compare the SUB simulation to two coarser resolution (10 km) simulations, one that includes a mixed layer eddy parameterization (MLE) and another that prescribes the restratification from SUB and advects the biogeochemical tracers using geostrophic velocities (NVF). The MLE simulates restratification of the mixed layer and bloom onset, but the spring bloom has a deficit of 10–13% in the new production compared to SUB. The NVF has the same restratification as SUB, and with no vertical flux of nutrients, leads to a spring bloom with a 32–40% new production deficit compared to SUB. Submesoscale processes lead to exchange across the mixed layer base, which is not represented in coarse resolution model simulations, even with mixed layer eddy parameterizations. Our results show that nutrients supplied by mixed layer eddies are important to enhance the spring bloom.",
}


@article{simoessousa2022a,
  title={Atmospheric Cold Pools in the Bay of Bengal},
  author={Simoes-Sousa, Iury T and Tandon, Amit and Buckley, Jared and Sengupta, Debasis and Shroyer, Emily and de Szoeke, Simon P},
  journal={Journal of the Atmospheric Sciences},
  doi={10.1175/JAS-D-22-0041.1},
  url={https://doi.org/10.1175/JAS-D-22-0041.1},
  year={2022},
  abstract="Atmospheric cold pools, generated by evaporative downdrafts from precipitating clouds, are ubiquitous in the Bay of Bengal. We use data from three moorings near 18°N to characterize a total of 465 cold pools. The cold pools are all dry, with a typical temperature drop of 2°C (max. 5°C) and specific humidity drop of 1 g/kg (max. 6 g/kg). Most cold pools last 1.5-3.5 hours (max. 14 hours). Cold pools occur almost every day in the North Bay from April to November, principally in the late morning, associated with intense precipitation that accounts for 80% of total rain. They increase the latent heat flux to the atmosphere by about 32 W/m2(median), although the instantaneous enhancement of latent heat flux for individual cold pools reaches 150 W/m2 . During the rainiest month (July), the cold pools occur 21% of the time and contribute nearly 14% to the mean evaporation. A composite analysis of all cold pools shows that the temperature and specific humidity anomalies are responsible for ~90% of the enhancement of sensible and latent heat flux, while variations in wind speed are responsible for the remainder. Depending on their gust front speed, the estimated height of the cold pools primarily ranges from 850 to 3200 m, with taller fronts more likely to occur during the summer monsoon season (Jun-Sep). Our results indicate that the realistic representation of cold pools in climate models is likely to be important for improved simulation of air-sea fluxes and monsoon rainfall."
}


@article{rocha2022,
  title={Compact Mesoscale Eddies in the South Brazil Bight},
  author={Rocha, Cesar B and Simoes-Sousa, Iury T},
  journal={Remote Sensing},
  volume={14},
  number={22},
  pages={5781},
  year={2022},
  publisher={MDPI},
  doi={10.3390/rs14225781},
  url={https://doi.org/10.3390/rs14225781},
  abstract="Recent studies suggest that the South Brazil Bight (SBB) hosts strong westward propagating mesoscale eddies. We use 28 years of satellite altimetry data and a new Eddy Atlas to estimate how much of the eddy kinetic energy (EKE) observed in the SBB is accounted for by local eddies, generated in the Brazil Current (BC) region, versus remote eddies generated eastward of the BC region. First, we estimate a BC frontal density to obtain a robust definition of BC region. The BC front is well-defined throughout the SBB, occupying the region between the 200-m and 1000-m isobath, except in eddy hotspots downstream of sharp inflections of the continental slope, where the EKE far exceeds the mean kinetic energy (MKE). Compact, closed-contour mesoscale eddies account for 30–50% of the total EKE observed in the SBB, with local eddies accounting for most of the compact EKE in the BC region, defined as the area within 200 km of the 28-year mean BC front. Remote compact eddies account for less than 10% of the EKE observed in the BC region; compact eddies generated at long distances from the SBB, including eddies generated in the Southeastern Atlantic, contribute an insignificant fraction of EKE in the BC region.",
}


@article{simoes2021barreirinhas,
  title={The Barreirinhas Eddies: Stable energetic anticyclones in the near-equatorial South Atlantic},
  author={Simoes-Sousa, Iury T and Silveira, Ilson Carlos A and Tandon, Amit and Flierl, Glenn R and Ribeiro, Cesar HA and Martins, Renato P},
  journal={Frontiers in Marine Science},
  url = {https://doi.org/10.3389/fmars.2021.617011},
  doi = {10.3389/fmars.2021.617011},
  volume={8},
  pages={28},
  year={2021},
  publisher={Frontiers},
  abstract="We explore the Barreirinhas Eddies, submesoscale vortices generated by the North Brazil Current (NBC) off the Barreirinhas Bight (Brazil, centered at 1.75°S), using vessel-mounted and moored ADCP data, and a Global HYCOM reanalysis. These double-stacked anticyclones with incredibly high Rossby Number [O(10)] occur independently at different depths (high Burger number). Anticyclones with Rossby number greater than unity are unstable according to inviscid linear theory, and hence these submesoscale features are not easily observable at mid latitudes. At these low latitudes, they last about a week, allowing characterization by oceanographic surveys. Our analyses suggest this increased stability is due to the joint effect of strong winds, stratification, proximity to the equator, and topography. Heretofore hypothesized via analytical studies and seen in numerical models, our study confirms this stabilization process in observations, and is also a starting point for the description of the submesoscale dynamics in the NBC domain.",
}


@article{napolitano2021can,
  title={Can the Intermediate Western Boundary Current recirculation trigger the Vit{\'o}ria Eddy formation?},
  author={Napolitano, Dante C and Rocha, Cesar B and da Silveira, Ilson CA and Simoes-Sousa, Iury T and Flierl, Glenn R},
  journal={Ocean Dynamics},
  url = {https://doi.org/10.1007/s10236-020-01437-6},
  doi = {10.1007/s10236-020-01437-6},
  volume={71},
  number={3},
  pages={281--292},
  year={2021},
  publisher={Springer Berlin Heidelberg},
  abstract="South of the Vitória-Trindade Ridge, a seamount chain off East Brazil, the Brazil Current (BC) meanders cyclonically within Tubarão Bight, occasionally forming the Vitória Eddy. It was recently found that the Intermediate Western Boundary Current (IWBC), which flows equatorward below the BC, cyclonically recirculate within Tubarão Bight. We present an analysis of AVISO observations that suggest that the Vitória Eddy formation is conditioned by the strength of the BC upstream of Tubarão Bight. A weak BC is prone to local meandering and eddy formation in the bight, while a strong BC suppresses eddy formation in the bight but triggers downstream meander growth. To study the effects of the IWBC recirculation on the BC meandering and the Vitória Eddy formation, we formulate a simple two-layer quasi-geostrophic model. In the model, the BC is represented by a meridional jet in the upper layer and the IWBC recirculation is a steady eddy in the lower layer. The lower-layer eddy effectively acts as a topographic bump, affecting the upper-layer jet via the stretching term \(\psi _{2}/{R_{d}^{2}}\), where ψ2 is the lower-layer streamfunction and Rd is the baroclinic deformation radius. Based on the AVISO sea-surface height data and previous observational studies, we define a stationary eddy and reference jet. We conduct a number of initial-value problem experiments varying the upper-layer jet speed. A weak upper-layer jet slowly meanders and develops a cyclone above the lower-layer eddy. As we increase the jet velocity, the meandering is faster and the cyclone is larger. But a too-strong jet has an opposite effect: the potential vorticity anomalies induced by the lower-layer eddy are quickly swept away, leading to explosive downstream meander growth; no cyclone is formed above the lower-layer eddy. In all cases, the initial meandering trigger is a linear process (the steering of the upper-layer jet by the lower-layer eddy). But even when the upper-layer jet is weak, nonlinearity quickly becomes important, dominating the dynamics after 10 days of simulation. The downstream meander growth is fully nonlinear. Our idealized QG model confirms that the IWBC recirculation can trigger the Vitória Eddy formation and elucidates the mechanisms involved in this process.",
}


@article{shroyer2021bay,
  title={Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset},
  author={Shroyer, Emily and Tandon, Amit and Sengupta, Debasis and Fernando, Harindra JS and Lucas, Andrew J and Farrar, J Thomas and Chattopadhyay, Rajib and de Szoeke, Simon and Flatau, Maria and Rydbeck, Adam and others},
  journal={Bulletin of the American Meteorological Society},
  url = {https://doi.org/10.1175/BAMS-D-20-0113.1},
  doi = {10.1175/BAMS-D-20-0113.1},
  pages={1--44},
  year={2021},
  abstract="In the Bay of Bengal, the warm, dry boreal spring concludes with the onset of the summer monsoon and accompanying southwesterly winds, heavy rains, and variable air-sea fluxes. Here, we summarize the 2018 monsoon onset using observations collected through the multinational Monsoon Intraseasonal Oscillations in the Bay of Bengal (MISO-BoB) program between the US, India, and Sri Lanka. MISO-BoB aims to improve understanding of monsoon intraseasonal variability, and the 2018 field effort captured the coupled air-sea response during a transition from active-to-break conditions in the central BoB. The active phase of the ~20-day research cruise was characterized by warm sea surface temperature (SST > 30°C), cold atmospheric outflows with intermittent heavy rainfall, and increasing winds (from 2 to 15 m s−1). Accumulated rainfall exceeded 200 mm with 90\% of precipitation occurring during the first week. The following break period was both dry and clear, with persistent 10−12 m s−1 wind and evaporation of 0.2 mm h−1. The evolving environmental state included a deepening ocean mixed layer (from ~20 to 50 m), cooling SST (by ~ 1°C), and warming/drying of the lower to mid-troposphere. Local atmospheric development was consistent with phasing of the large-scale intraseasonal oscillation. The upper ocean stores significant heat in the BoB, enough to maintain SST above 29°C despite cooling by surface fluxes and ocean mixing. Comparison with reanalysis indicates biases in air-sea fluxes, which may be related to overly cool prescribed SST. Resolution of such biases offers a path toward improved forecasting of transition periods in the monsoon.",
}


@article{luko2021revisiting,
  title={Revisiting the Atlantic South Equatorial Current},
  author={Luko, CD and da Silveira, ICA and Simoes-Sousa, IT and Araujo, JM and Tandon, A},
  journal={Journal of Geophysical Research: Oceans},
  pages={e2021JC017387},
  url = {https://doi.org/10.1029/2021JC017387},
  doi = {10.1029/2021JC017387},
  year={2021},
  abstract="The southern branch of the South Equatorial Current (SSEC) is the northern limit of the South Atlantic Subtropical Gyre. When this current reaches Brazil around 14°S it bifurcates into a southward flow as the Brazil Current (BC) and the surface portion of the northward flowing North Brazil Undercurrent (NBUC). The SSEC system is a key component of the western boundary supply, influencing the NBUC/BC variability and, therefore, global climate through the Meridional Overturning Circulation. In this study, using altimetry satellite data and reanalyzes outputs (1993–2018), we revisit the SSEC mean state and show this current arriving at the South Atlantic western boundary as a multi-banded flow with surface signatures resulting from different subsurface cores. These bands have velocities between 0.02 and 0.07 m s$^{−1}$ and, as shown by ADCP data from the PIRATA project, their signature in synoptic scenarios is obscured by eddies and waves with velocities between 0.1 and 0.3 m s$^{−1}$. In addition, the SSEC annual cycle analysis shows that the seasonality of the bands is out of phase with each other, presenting westward transport anomalies between 0.4 and 2.6 Sv. Finally, our results show that the seasonality of this multi-banded flow both defines where the BC is born, and modulates the seasonality of semi-permanent mesoscale eddies off Brazil.",
}


@article{polito2021,
  title = {Insights on the non-linear solution of Munk's ocean circulation theory from a rotating tank experiment},
  author = {Paulo S. Polito and Olga T. Sato and Dante C. Napolitano and Iury T. Simoes-Sousa and Helio Almeida and Fabricio R. Lapolli},
  journal = {Ocean and Coastal Research},
  doi = {10.1590/2675-2824069.20-011psp},
  url = {https://doi.org/10.1590/2675-2824069.20-011psp},
  year = {2021},
  publisher = {{FapUNIFESP} ({SciELO})},
  volume = {69},
  abstract = "At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk's circulation theory aided by a Lagrangian particles tracking algorithm and numerical modeling. From information captured by video, we track the trajectories of drifters, and then objectively mapped the streamfunction to obtain the mean circulation pattern. We were able to reproduce the wind-forced anticyclonic and asymmetric gyre, including the western boundary intensification and its retroflection. The latter phenomenon was predicted by the non-linear version of Munk's model and observed in real subtropical gyres as small recirculation regions. We have configured two numerical model simulations mimicking the physical experiment, with linear and non-linear terms. The comparison between the numerical and physical experiments confirmed the effect of non-linear distortion of the gyre. Geophysical fluid dynamics is often hard to visualize, and counter-intuitive in a rotating system. We present this set of experiments as a tool for oceanography teaching. Besides studying general ocean circulation theories and observations through practical examples, this experiment provides an opportunity to develop basic image processing and geophysical modelling skills.",
}


@article{santin2019biological,
  title={Biological and Toxicological Evaluation of N-(4methyl-phenyl)-4-methylphthalimide on Bone Cancer in Mice},
  author={Santin, Jose R and da Silva, Gislaine F and Pastor, Maria VD and Broering, Milena F and Nunes, Roberta and Braga, Rodolpho C and Simoes-Sousa, Iury T. and Stiz, Dorimar S and da Silva, Kathryn ABS and Stoeberl, Luis C and others},
  journal={Anti-Cancer Agents in Medicinal Chemistry (Formerly Current Medicinal Chemistry-Anti-Cancer Agents)},
  url = {https://doi.org/10.2174/1871520619666190207130732},
  doi = {10.2174/1871520619666190207130732},
  volume={19},
  number={5},
  pages={667--676},
  year={2019},
  publisher={Bentham Science Publishers}
}


@article{marseal2018,
  title = {As Correntes Oceânicas na {Bacia Sergipe-Alagoas}},
  author = {Ilson Silveira and Dante Napolitano and Iury Simoes-Sousa and Renato Parkinson and Wandrey Watanabe},
  journal = {Revista Marseal: Edição Águas Profundas SE/AL},
  year = {2018},
  volume = {2},
  pages = {36--39},
  issn = {2596-0547},
  publisher = {Editora UFS e Centro de Pesquisas da Petrobras (CENPES)},
  url = {https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/}
}


@article{carvalho2023,
  title = {Surfing the currents: {T}he longest distance traveled by a released {W}est {I}ndian manatee (\textit{{T}richechus manatus}) and the implications for conservation},
  author = {Carvalho, Camila and Simoes-Sousa, Iury Tercio and Santos, Lucas Pereira and Choi-Lima, Katherine Fiedler and Pereira, Letícia Gonçalves and Alves, Maria Danise de Oliveira and Carrero, Adrian and Santander, Juan Carlos and Carvalho, Vitor Luz},
  journal = {Journal of the Marine Biological Association of the United Kingdom},
  year = {2023},
  note = {Under review.},
  issn = {1469-7769}
}
\">\n            <i class=\"fa fa-download fa-fw\"></i> Download BibTeX\n          </a>\n        </li>\n        <li>\n          <a href=\"//bibbase.org/rss?bib=https://iuryt.github.io/pubs.bib\">\n            <i class=\"fa fa-rss fa-fw\"></i> RSS Feed\n          </a>\n          </li>\n      </ul>\n      </li>\n\n      \n\n\n      \n    </ul>\n\n\n    <div class=\"alert alert-success bibbase_msg\" id=\"bibbase_msg_embed\"\n         style=\"display: none;\">\n\n      Excellent! 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In order to keep using Mendeley with BibBase past April\n        14th, you need to:\n        <ol>\n          <li>renew the authorization for BibBase on Mendeley, and</li>\n          <li>update the BibBase URL\n            in your page the same way you did when you initially set up\n            this page.\n          </li>\n        </ol>\n      </p>\n\n      <p>\n        <a href=\"http://bibbase.org/cgi-bin/mendeley2/get.py\">\n          <i class=\"fa fa-angle-double-right\"></i>\n          Fix it now</a>\n      </p>\n    </div>\n\n  </div>\n\n\n  <div id=\"bibbase_body\">\n    \n  \n  <div class=\"bibbase_group_whole\" id=\"group_2023\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2023')\"\n      onkeypress=\"toggleGroup('group_2023')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2023</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"carvalho-simoessousa-santos-choilima-pereira-alves-carrero-santander-etal-surfingthecurrentsthelongestdistancetraveledbyareleasedwestindianmanateeitrichechusmanatusiandtheimplicationsforconservation-2023\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Surfing the currents: The longest distance traveled by a released West Indian manatee (<i>Trichechus manatus</i>) and the implications for conservation.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Carvalho, C.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T.</a>; Santos, L. P.; Choi-Lima, K. F.; Pereira, L. G.; Alves, M. D. d. O.; Carrero, A.; Santander, J. C.;  and Carvalho, V. L.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of the Marine Biological Association of the United Kingdom</i>.  2023.\n  <span class=\"note\">Under review.</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/carvalho-simoessousa-santos-choilima-pereira-alves-carrero-santander-etal-surfingthecurrentsthelongestdistancetraveledbyareleasedwestindianmanateeitrichechusmanatusiandtheimplicationsforconservation-2023\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('carvalho-simoessousa-santos-choilima-pereira-alves-carrero-santander-etal-surfingthecurrentsthelongestdistancetraveledbyareleasedwestindianmanateeitrichechusmanatusiandtheimplicationsforconservation-2023')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{carvalho2023,\n  title = {Surfing the currents: {T}he longest distance traveled by a released {W}est {I}ndian manatee (\\textit{{T}richechus manatus}) and the implications for conservation},\n  author = {Carvalho, Camila and Simoes-Sousa, Iury Tercio and Santos, Lucas Pereira and Choi-Lima, Katherine Fiedler and Pereira, Letícia Gonçalves and Alves, Maria Danise de Oliveira and Carrero, Adrian and Santander, Juan Carlos and Carvalho, Vitor Luz},\n  journal = {Journal of the Marine Biological Association of the United Kingdom},\n  year = {2023},\n  note = {Under review.},\n  issn = {1469-7769}\n}\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2022\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2022')\"\n      onkeypress=\"toggleGroup('group_2022')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2022</span>\n      <span class=\"bibbase_group_count\">\n        \n        (5)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://www.sciencedirect.com/science/article/pii/S0079661122001847\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022', 'https://www.sciencedirect.com/science/article/pii/S0079661122001847', event);\">\n    The Brazil Current quasi-stationary unstable meanders at 22°S–23°S.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Silveira, I. C.; Pereira, F.; Flierl, G. R.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T.</a>; Palóczy, A.; Borges-Silva, M.;  and Rocha, C. B.\n</span>\n\n  \n\n</span>\n\n  <i>Progress in Oceanography</i>,102925.  2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://www.sciencedirect.com/science/article/pii/S0079661122001847\"\n     onclick=\"log_download('silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022', 'https://www.sciencedirect.com/science/article/pii/S0079661122001847', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The Brazil Current quasi-stationary unstable meanders at 22°S–23°S [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/https://doi.org/10.1016/j.pocean.2022.102925\"\n     onclick=\"log_download('silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022', 'http://doi.org/https://doi.org/10.1016/j.pocean.2022.102925', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('silveira-pereira-flierl-simoessousa-palczy-borgessilva-rocha-thebrazilcurrentquasistationaryunstablemeandersat22s23s-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{silveira2022,\ntitle = {The Brazil Current quasi-stationary unstable meanders at 22°S–23°S},\njournal = {Progress in Oceanography},\npages = {102925},\nyear = {2022},\nissn = {0079-6611},\ndoi = {https://doi.org/10.1016/j.pocean.2022.102925},\nurl = {https://www.sciencedirect.com/science/article/pii/S0079661122001847},\nauthor = {Ilson C.A. {Silveira} and Filipe Pereira and Glenn R. Flierl and Iury T. Simoes-Sousa and André Palóczy and Milton Borges-Silva and César B. Rocha},\nkeywords = {Brazil current, Baroclinic instability, Mesoscale eddies, Western boundary currents, Conservation of potential vorticity, Contour dynamics, South Atlantic, Cape Frio, Cape São Tomé},\nabstract = {The most conspicuous oceanographic features off Southeastern Brazil are the quasi-stationary eddies formed off Capes São Tomé (CSTE) and Frio (CFE) associated with the Brazil Current (BC). We use SST and SSH products to infer eddy growth rates. These two independent data sets reveal an average growth rate of 0.06day-1, and propagation speeds are virtually null. CFE tends to be more unstable and frequent than CSTE (3.5 vs. 2.3 events per year). CSTE can propagate toward the north or south while CFE only propagates southward. We perform potential vorticity (PV) inversion calculation using hydrographic data to understand how the meander growth occurs in the baroclinic jet formed by the BC and the Intermediate Western Boundary Current (IWBC). PV anomalies in one layer enhanced the anomalies on the other. This result offered in situ evidence of baroclinic conversion occurring during the eddy event captured in the observations. We then build a theoretical two-layer model calibrated with the observations seeking to explain why the eddies grow in place, and no accompanying unstable anticyclones are formed. The experiments lead us to conclude that the eddies’ quasi-stationarity is due to the almost pure baroclinic nature of the BC-IWBC jet. We also find that the western boundary inhibits the formation of the anticyclones. As observed in satellite imagery, the meanders develop as isolated disturbances that may grow simultaneously or not.}\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The most conspicuous oceanographic features off Southeastern Brazil are the quasi-stationary eddies formed off Capes São Tomé (CSTE) and Frio (CFE) associated with the Brazil Current (BC). We use SST and SSH products to infer eddy growth rates. These two independent data sets reveal an average growth rate of 0.06day-1, and propagation speeds are virtually null. CFE tends to be more unstable and frequent than CSTE (3.5 vs. 2.3 events per year). CSTE can propagate toward the north or south while CFE only propagates southward. We perform potential vorticity (PV) inversion calculation using hydrographic data to understand how the meander growth occurs in the baroclinic jet formed by the BC and the Intermediate Western Boundary Current (IWBC). PV anomalies in one layer enhanced the anomalies on the other. This result offered in situ evidence of baroclinic conversion occurring during the eddy event captured in the observations. We then build a theoretical two-layer model calibrated with the observations seeking to explain why the eddies grow in place, and no accompanying unstable anticyclones are formed. The experiments lead us to conclude that the eddies’ quasi-stationarity is due to the almost pure baroclinic nature of the BC-IWBC jet. We also find that the western boundary inhibits the formation of the anticyclones. As observed in satellite imagery, the meanders develop as isolated disturbances that may grow simultaneously or not.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://www.sciencedirect.com/science/article/pii/S0967063722002606\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022', 'https://www.sciencedirect.com/science/article/pii/S0967063722002606', event);\">\n    The Brazil Current mesoscale eddies: Altimetry-based characterization and tracking.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Uchoa, I.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T.</a>;  and da Silveira , I. C.\n</span>\n\n  \n\n</span>\n\n  <i>Deep Sea Research Part I: Oceanographic Research Papers</i>,103947.  2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://www.sciencedirect.com/science/article/pii/S0967063722002606\"\n     onclick=\"log_download('uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022', 'https://www.sciencedirect.com/science/article/pii/S0967063722002606', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The Brazil Current mesoscale eddies: Altimetry-based characterization and tracking [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.dsr.2022.103947\"\n     onclick=\"log_download('uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022', 'http://doi.org/10.1016/j.dsr.2022.103947', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('uchoa-simoessousa-dasilveira-thebrazilcurrentmesoscaleeddiesaltimetrybasedcharacterizationandtracking-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{uchoa2022,\ntitle = {The Brazil Current mesoscale eddies: Altimetry-based characterization and tracking},\njournal = {Deep Sea Research Part I: Oceanographic Research Papers},\npages = {103947},\nyear = {2022},\nissn = {0967-0637},\ndoi = {10.1016/j.dsr.2022.103947},\nurl = {https://www.sciencedirect.com/science/article/pii/S0967063722002606},\nauthor = {Igor Uchoa and Iury T. Simoes-Sousa and Ilson C.A. {da Silveira}},\nkeywords = {Eddy detection algorithm, Western boundary current, Brazil Current, South Atlantic, Mesoscale eddies, Altimetry},\nabstract = {The Brazil Current (BC) has been reported as eddy-dominated, with recurrent formation of eddies and meanders along the margin. In this study, we characterize the variability of mesoscale eddies associated with this western boundary current from its origin site to the southern end of the South Brazil Bight (∼15°S – ∼28°S). We apply an eddy detection method on a 27-year multi-satellite altimetry product. We offer a first quantitative estimate of the eddy dominance along the BC path. On average, there are no major differences in the eddy parameters between cyclones and anticyclones. However, north of the 20∘S, the eddies are larger and slower in swirling speed, whereas the opposite patterns occur with the eddies south of 20∘S. Although there is no notable seasonality in the eddy formation in general, there is a tendency to form cyclones in the vicinity of capes and bights of the southeastern Brazilian shelfbreak. In contrast, there is a scattered horizontal distribution of anticyclone formation for most of the BC domain throughout the seasons. The Vitória, Cape São Tomé and Cape Frio Eddies account for ∼30% of the total cyclones in the analysis. The Vitória Eddy (VE) tends to be more often generated in austral autumn, the season of lowest kinetic energy and volume transport of the BC. The Cape São Tomé Eddy (CSTE) and Cape Frio Eddy (CFE) are more energetic in the seasons of the BC’s highest volume transport (austral spring and summer). Despite most of the eddies being described as quasi-stationary in the current literature, our analysis of the eddy trajectories showed that the VE, CFE and CSTE can detach and migrate off of the mean BC axis. We estimate that ∼30% of the CFE events pinch off and migrate southwestward. The CSTE and CFE presented the highest growth rates (0.08 and 0.07 day−1 , respectively) of the recurrent eddies. These results provide a first robust characterization of the BC mesoscale eddies.}\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The Brazil Current (BC) has been reported as eddy-dominated, with recurrent formation of eddies and meanders along the margin. In this study, we characterize the variability of mesoscale eddies associated with this western boundary current from its origin site to the southern end of the South Brazil Bight (∼15°S – ∼28°S). We apply an eddy detection method on a 27-year multi-satellite altimetry product. We offer a first quantitative estimate of the eddy dominance along the BC path. On average, there are no major differences in the eddy parameters between cyclones and anticyclones. However, north of the 20∘S, the eddies are larger and slower in swirling speed, whereas the opposite patterns occur with the eddies south of 20∘S. Although there is no notable seasonality in the eddy formation in general, there is a tendency to form cyclones in the vicinity of capes and bights of the southeastern Brazilian shelfbreak. In contrast, there is a scattered horizontal distribution of anticyclone formation for most of the BC domain throughout the seasons. The Vitória, Cape São Tomé and Cape Frio Eddies account for ∼30% of the total cyclones in the analysis. The Vitória Eddy (VE) tends to be more often generated in austral autumn, the season of lowest kinetic energy and volume transport of the BC. The Cape São Tomé Eddy (CSTE) and Cape Frio Eddy (CFE) are more energetic in the seasons of the BC’s highest volume transport (austral spring and summer). Despite most of the eddies being described as quasi-stationary in the current literature, our analysis of the eddy trajectories showed that the VE, CFE and CSTE can detach and migrate off of the mean BC axis. We estimate that ∼30% of the CFE events pinch off and migrate southwestward. The CSTE and CFE presented the highest growth rates (0.08 and 0.07 day−1 , respectively) of the recurrent eddies. These results provide a first robust characterization of the BC mesoscale eddies.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.3389/fmars.2022.825027\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022', 'https://doi.org/10.3389/fmars.2022.825027', event);\">\n    Mixed layer eddies supply nutrients to enhance the spring phytoplankton bloom.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T.</a>; Tandon, A.; Pereira, F.; Lazaneo, C. Z.;  and Mahadevan, A.\n</span>\n\n  \n\n</span>\n\n  <i>Frontiers in Marine Science</i>, 9.  2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.3389/fmars.2022.825027\"\n     onclick=\"log_download('simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022', 'https://doi.org/10.3389/fmars.2022.825027', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Mixed layer eddies supply nutrients to enhance the spring phytoplankton bloom [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.3389/fmars.2022.825027\"\n     onclick=\"log_download('simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022', 'http://doi.org/10.3389/fmars.2022.825027', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('simoessousa-tandon-pereira-lazaneo-mahadevan-mixedlayereddiessupplynutrientstoenhancethespringphytoplanktonbloom-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@ARTICLE{simoessousa2022b,\nAUTHOR={Simoes-Sousa, Iury T. and Tandon, Amit and Pereira, Filipe and Lazaneo, Caue Z. and Mahadevan, Amala},   \nTITLE={Mixed layer eddies supply nutrients to enhance the spring phytoplankton bloom},      \nJOURNAL={Frontiers in Marine Science},      \nVOLUME={9},           \nYEAR={2022},        \nURL={https://www.frontiersin.org/articles/10.3389/fmars.2022.825027},       \nDOI={10.3389/fmars.2022.825027},\nURL={https://doi.org/10.3389/fmars.2022.825027},\nISSN={2296-7745},\nabstract=&quot;Mixed layer eddies resulting from baroclinic instability of fronts convert horizontal buoyancy gradients into vertical stratification, shoaling the mixed layer. In light-limited regimes – high-latitudes – this process can initiate phytoplankton blooms prior to the springtime warming. The question is whether mixed layer eddies can enhance the spring bloom by delivering nutrients from beneath the mixed layer. We couple a submesoscale-resolving model (SUB) with a simple ecosystem model and examine the role of mixed layer eddies on the development of the spring bloom. We compare the SUB simulation to two coarser resolution (10 km) simulations, one that includes a mixed layer eddy parameterization (MLE) and another that prescribes the restratification from SUB and advects the biogeochemical tracers using geostrophic velocities (NVF). The MLE simulates restratification of the mixed layer and bloom onset, but the spring bloom has a deficit of 10–13% in the new production compared to SUB. The NVF has the same restratification as SUB, and with no vertical flux of nutrients, leads to a spring bloom with a 32–40% new production deficit compared to SUB. Submesoscale processes lead to exchange across the mixed layer base, which is not represented in coarse resolution model simulations, even with mixed layer eddy parameterizations. Our results show that nutrients supplied by mixed layer eddies are important to enhance the spring bloom.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Mixed layer eddies resulting from baroclinic instability of fronts convert horizontal buoyancy gradients into vertical stratification, shoaling the mixed layer. In light-limited regimes – high-latitudes – this process can initiate phytoplankton blooms prior to the springtime warming. The question is whether mixed layer eddies can enhance the spring bloom by delivering nutrients from beneath the mixed layer. We couple a submesoscale-resolving model (SUB) with a simple ecosystem model and examine the role of mixed layer eddies on the development of the spring bloom. We compare the SUB simulation to two coarser resolution (10 km) simulations, one that includes a mixed layer eddy parameterization (MLE) and another that prescribes the restratification from SUB and advects the biogeochemical tracers using geostrophic velocities (NVF). The MLE simulates restratification of the mixed layer and bloom onset, but the spring bloom has a deficit of 10–13% in the new production compared to SUB. The NVF has the same restratification as SUB, and with no vertical flux of nutrients, leads to a spring bloom with a 32–40% new production deficit compared to SUB. Submesoscale processes lead to exchange across the mixed layer base, which is not represented in coarse resolution model simulations, even with mixed layer eddy parameterizations. Our results show that nutrients supplied by mixed layer eddies are important to enhance the spring bloom.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1175/JAS-D-22-0041.1\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022', 'https://doi.org/10.1175/JAS-D-22-0041.1', event);\">\n    Atmospheric Cold Pools in the Bay of Bengal.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T</a>; Tandon, A.; Buckley, J.; Sengupta, D.; Shroyer, E.;  and de Szoeke, S. P\n</span>\n\n  \n\n</span>\n\n  <i>Journal of the Atmospheric Sciences</i>.  2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1175/JAS-D-22-0041.1\"\n     onclick=\"log_download('simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022', 'https://doi.org/10.1175/JAS-D-22-0041.1', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Atmospheric Cold Pools in the Bay of Bengal [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1175/JAS-D-22-0041.1\"\n     onclick=\"log_download('simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022', 'http://doi.org/10.1175/JAS-D-22-0041.1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('simoessousa-tandon-buckley-sengupta-shroyer-deszoeke-atmosphericcoldpoolsinthebayofbengal-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{simoessousa2022a,\n  title={Atmospheric Cold Pools in the Bay of Bengal},\n  author={Simoes-Sousa, Iury T and Tandon, Amit and Buckley, Jared and Sengupta, Debasis and Shroyer, Emily and de Szoeke, Simon P},\n  journal={Journal of the Atmospheric Sciences},\n  doi={10.1175/JAS-D-22-0041.1},\n  url={https://doi.org/10.1175/JAS-D-22-0041.1},\n  year={2022},\n  abstract=&quot;Atmospheric cold pools, generated by evaporative downdrafts from precipitating clouds, are ubiquitous in the Bay of Bengal. We use data from three moorings near 18°N to characterize a total of 465 cold pools. The cold pools are all dry, with a typical temperature drop of 2°C (max. 5°C) and specific humidity drop of 1 g/kg (max. 6 g/kg). Most cold pools last 1.5-3.5 hours (max. 14 hours). Cold pools occur almost every day in the North Bay from April to November, principally in the late morning, associated with intense precipitation that accounts for 80% of total rain. They increase the latent heat flux to the atmosphere by about 32 W/m2(median), although the instantaneous enhancement of latent heat flux for individual cold pools reaches 150 W/m2 . During the rainiest month (July), the cold pools occur 21% of the time and contribute nearly 14% to the mean evaporation. A composite analysis of all cold pools shows that the temperature and specific humidity anomalies are responsible for ~90% of the enhancement of sensible and latent heat flux, while variations in wind speed are responsible for the remainder. Depending on their gust front speed, the estimated height of the cold pools primarily ranges from 850 to 3200 m, with taller fronts more likely to occur during the summer monsoon season (Jun-Sep). Our results indicate that the realistic representation of cold pools in climate models is likely to be important for improved simulation of air-sea fluxes and monsoon rainfall.&quot;\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Atmospheric cold pools, generated by evaporative downdrafts from precipitating clouds, are ubiquitous in the Bay of Bengal. We use data from three moorings near 18°N to characterize a total of 465 cold pools. The cold pools are all dry, with a typical temperature drop of 2°C (max. 5°C) and specific humidity drop of 1 g/kg (max. 6 g/kg). Most cold pools last 1.5-3.5 hours (max. 14 hours). Cold pools occur almost every day in the North Bay from April to November, principally in the late morning, associated with intense precipitation that accounts for 80% of total rain. They increase the latent heat flux to the atmosphere by about 32 W/m2(median), although the instantaneous enhancement of latent heat flux for individual cold pools reaches 150 W/m2 . During the rainiest month (July), the cold pools occur 21% of the time and contribute nearly 14% to the mean evaporation. A composite analysis of all cold pools shows that the temperature and specific humidity anomalies are responsible for  90% of the enhancement of sensible and latent heat flux, while variations in wind speed are responsible for the remainder. Depending on their gust front speed, the estimated height of the cold pools primarily ranges from 850 to 3200 m, with taller fronts more likely to occur during the summer monsoon season (Jun-Sep). Our results indicate that the realistic representation of cold pools in climate models is likely to be important for improved simulation of air-sea fluxes and monsoon rainfall.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.3390/rs14225781\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022', 'https://doi.org/10.3390/rs14225781', event);\">\n    Compact Mesoscale Eddies in the South Brazil Bight.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Rocha, C. B;  and <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T</a>\n</span>\n\n  \n\n</span>\n\n  <i>Remote Sensing</i>, 14(22): 5781.  2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.3390/rs14225781\"\n     onclick=\"log_download('rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022', 'https://doi.org/10.3390/rs14225781', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Compact Mesoscale Eddies in the South Brazil Bight [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.3390/rs14225781\"\n     onclick=\"log_download('rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022', 'http://doi.org/10.3390/rs14225781', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('rocha-simoessousa-compactmesoscaleeddiesinthesouthbrazilbight-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{rocha2022,\n  title={Compact Mesoscale Eddies in the South Brazil Bight},\n  author={Rocha, Cesar B and Simoes-Sousa, Iury T},\n  journal={Remote Sensing},\n  volume={14},\n  number={22},\n  pages={5781},\n  year={2022},\n  publisher={MDPI},\n  doi={10.3390/rs14225781},\n  url={https://doi.org/10.3390/rs14225781},\n  abstract=&quot;Recent studies suggest that the South Brazil Bight (SBB) hosts strong westward propagating mesoscale eddies. We use 28 years of satellite altimetry data and a new Eddy Atlas to estimate how much of the eddy kinetic energy (EKE) observed in the SBB is accounted for by local eddies, generated in the Brazil Current (BC) region, versus remote eddies generated eastward of the BC region. First, we estimate a BC frontal density to obtain a robust definition of BC region. The BC front is well-defined throughout the SBB, occupying the region between the 200-m and 1000-m isobath, except in eddy hotspots downstream of sharp inflections of the continental slope, where the EKE far exceeds the mean kinetic energy (MKE). Compact, closed-contour mesoscale eddies account for 30–50% of the total EKE observed in the SBB, with local eddies accounting for most of the compact EKE in the BC region, defined as the area within 200 km of the 28-year mean BC front. Remote compact eddies account for less than 10% of the EKE observed in the BC region; compact eddies generated at long distances from the SBB, including eddies generated in the Southeastern Atlantic, contribute an insignificant fraction of EKE in the BC region.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Recent studies suggest that the South Brazil Bight (SBB) hosts strong westward propagating mesoscale eddies. We use 28 years of satellite altimetry data and a new Eddy Atlas to estimate how much of the eddy kinetic energy (EKE) observed in the SBB is accounted for by local eddies, generated in the Brazil Current (BC) region, versus remote eddies generated eastward of the BC region. First, we estimate a BC frontal density to obtain a robust definition of BC region. The BC front is well-defined throughout the SBB, occupying the region between the 200-m and 1000-m isobath, except in eddy hotspots downstream of sharp inflections of the continental slope, where the EKE far exceeds the mean kinetic energy (MKE). Compact, closed-contour mesoscale eddies account for 30–50% of the total EKE observed in the SBB, with local eddies accounting for most of the compact EKE in the BC region, defined as the area within 200 km of the 28-year mean BC front. Remote compact eddies account for less than 10% of the EKE observed in the BC region; compact eddies generated at long distances from the SBB, including eddies generated in the Southeastern Atlantic, contribute an insignificant fraction of EKE in the BC region.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2021\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2021')\"\n      onkeypress=\"toggleGroup('group_2021')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2021</span>\n      <span class=\"bibbase_group_count\">\n        \n        (5)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.3389/fmars.2021.617011\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021', 'https://doi.org/10.3389/fmars.2021.617011', event);\">\n    The Barreirinhas Eddies: Stable energetic anticyclones in the near-equatorial South Atlantic.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T</a>; Silveira, I. C. A; Tandon, A.; Flierl, G. R; Ribeiro, C. H.;  and Martins, R. P\n</span>\n\n  \n\n</span>\n\n  <i>Frontiers in Marine Science</i>, 8: 28.  2021.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.3389/fmars.2021.617011\"\n     onclick=\"log_download('simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021', 'https://doi.org/10.3389/fmars.2021.617011', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The Barreirinhas Eddies: Stable energetic anticyclones in the near-equatorial South Atlantic [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.3389/fmars.2021.617011\"\n     onclick=\"log_download('simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021', 'http://doi.org/10.3389/fmars.2021.617011', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('simoessousa-silveira-tandon-flierl-ribeiro-martins-thebarreirinhaseddiesstableenergeticanticyclonesinthenearequatorialsouthatlantic-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{simoes2021barreirinhas,\n  title={The Barreirinhas Eddies: Stable energetic anticyclones in the near-equatorial South Atlantic},\n  author={Simoes-Sousa, Iury T and Silveira, Ilson Carlos A and Tandon, Amit and Flierl, Glenn R and Ribeiro, Cesar HA and Martins, Renato P},\n  journal={Frontiers in Marine Science},\n  url = {https://doi.org/10.3389/fmars.2021.617011},\n  doi = {10.3389/fmars.2021.617011},\n  volume={8},\n  pages={28},\n  year={2021},\n  publisher={Frontiers},\n  abstract=&quot;We explore the Barreirinhas Eddies, submesoscale vortices generated by the North Brazil Current (NBC) off the Barreirinhas Bight (Brazil, centered at 1.75°S), using vessel-mounted and moored ADCP data, and a Global HYCOM reanalysis. These double-stacked anticyclones with incredibly high Rossby Number [O(10)] occur independently at different depths (high Burger number). Anticyclones with Rossby number greater than unity are unstable according to inviscid linear theory, and hence these submesoscale features are not easily observable at mid latitudes. At these low latitudes, they last about a week, allowing characterization by oceanographic surveys. Our analyses suggest this increased stability is due to the joint effect of strong winds, stratification, proximity to the equator, and topography. Heretofore hypothesized via analytical studies and seen in numerical models, our study confirms this stabilization process in observations, and is also a starting point for the description of the submesoscale dynamics in the NBC domain.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  We explore the Barreirinhas Eddies, submesoscale vortices generated by the North Brazil Current (NBC) off the Barreirinhas Bight (Brazil, centered at 1.75°S), using vessel-mounted and moored ADCP data, and a Global HYCOM reanalysis. These double-stacked anticyclones with incredibly high Rossby Number [O(10)] occur independently at different depths (high Burger number). Anticyclones with Rossby number greater than unity are unstable according to inviscid linear theory, and hence these submesoscale features are not easily observable at mid latitudes. At these low latitudes, they last about a week, allowing characterization by oceanographic surveys. Our analyses suggest this increased stability is due to the joint effect of strong winds, stratification, proximity to the equator, and topography. Heretofore hypothesized via analytical studies and seen in numerical models, our study confirms this stabilization process in observations, and is also a starting point for the description of the submesoscale dynamics in the NBC domain.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1007/s10236-020-01437-6\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021', 'https://doi.org/10.1007/s10236-020-01437-6', event);\">\n    Can the Intermediate Western Boundary Current recirculation trigger the Vitória Eddy formation?.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Napolitano, D. C; Rocha, C. B; da Silveira, I. C.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T</a>;  and Flierl, G. R\n</span>\n\n  \n\n</span>\n\n  <i>Ocean Dynamics</i>, 71(3): 281–292.  2021.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1007/s10236-020-01437-6\"\n     onclick=\"log_download('napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021', 'https://doi.org/10.1007/s10236-020-01437-6', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Can the Intermediate Western Boundary Current recirculation trigger the Vitória Eddy formation? [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s10236-020-01437-6\"\n     onclick=\"log_download('napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021', 'http://doi.org/10.1007/s10236-020-01437-6', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('napolitano-rocha-dasilveira-simoessousa-flierl-cantheintermediatewesternboundarycurrentrecirculationtriggerthevitriaeddyformation-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{napolitano2021can,\n  title={Can the Intermediate Western Boundary Current recirculation trigger the Vit{\\&#x27;o}ria Eddy formation?},\n  author={Napolitano, Dante C and Rocha, Cesar B and da Silveira, Ilson CA and Simoes-Sousa, Iury T and Flierl, Glenn R},\n  journal={Ocean Dynamics},\n  url = {https://doi.org/10.1007/s10236-020-01437-6},\n  doi = {10.1007/s10236-020-01437-6},\n  volume={71},\n  number={3},\n  pages={281--292},\n  year={2021},\n  publisher={Springer Berlin Heidelberg},\n  abstract=&quot;South of the Vitória-Trindade Ridge, a seamount chain off East Brazil, the Brazil Current (BC) meanders cyclonically within Tubarão Bight, occasionally forming the Vitória Eddy. It was recently found that the Intermediate Western Boundary Current (IWBC), which flows equatorward below the BC, cyclonically recirculate within Tubarão Bight. We present an analysis of AVISO observations that suggest that the Vitória Eddy formation is conditioned by the strength of the BC upstream of Tubarão Bight. A weak BC is prone to local meandering and eddy formation in the bight, while a strong BC suppresses eddy formation in the bight but triggers downstream meander growth. To study the effects of the IWBC recirculation on the BC meandering and the Vitória Eddy formation, we formulate a simple two-layer quasi-geostrophic model. In the model, the BC is represented by a meridional jet in the upper layer and the IWBC recirculation is a steady eddy in the lower layer. The lower-layer eddy effectively acts as a topographic bump, affecting the upper-layer jet via the stretching term \\(\\psi _{2}/{R_{d}^{2}}\\), where ψ2 is the lower-layer streamfunction and Rd is the baroclinic deformation radius. Based on the AVISO sea-surface height data and previous observational studies, we define a stationary eddy and reference jet. We conduct a number of initial-value problem experiments varying the upper-layer jet speed. A weak upper-layer jet slowly meanders and develops a cyclone above the lower-layer eddy. As we increase the jet velocity, the meandering is faster and the cyclone is larger. But a too-strong jet has an opposite effect: the potential vorticity anomalies induced by the lower-layer eddy are quickly swept away, leading to explosive downstream meander growth; no cyclone is formed above the lower-layer eddy. In all cases, the initial meandering trigger is a linear process (the steering of the upper-layer jet by the lower-layer eddy). But even when the upper-layer jet is weak, nonlinearity quickly becomes important, dominating the dynamics after 10 days of simulation. The downstream meander growth is fully nonlinear. Our idealized QG model confirms that the IWBC recirculation can trigger the Vitória Eddy formation and elucidates the mechanisms involved in this process.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  South of the Vitória-Trindade Ridge, a seamount chain off East Brazil, the Brazil Current (BC) meanders cyclonically within Tubarão Bight, occasionally forming the Vitória Eddy. It was recently found that the Intermediate Western Boundary Current (IWBC), which flows equatorward below the BC, cyclonically recirculate within Tubarão Bight. We present an analysis of AVISO observations that suggest that the Vitória Eddy formation is conditioned by the strength of the BC upstream of Tubarão Bight. A weak BC is prone to local meandering and eddy formation in the bight, while a strong BC suppresses eddy formation in the bight but triggers downstream meander growth. To study the effects of the IWBC recirculation on the BC meandering and the Vitória Eddy formation, we formulate a simple two-layer quasi-geostrophic model. In the model, the BC is represented by a meridional jet in the upper layer and the IWBC recirculation is a steady eddy in the lower layer. The lower-layer eddy effectively acts as a topographic bump, affecting the upper-layer jet via the stretching term \\(ψ _2/R_d^2\\), where ψ2 is the lower-layer streamfunction and Rd is the baroclinic deformation radius. Based on the AVISO sea-surface height data and previous observational studies, we define a stationary eddy and reference jet. We conduct a number of initial-value problem experiments varying the upper-layer jet speed. A weak upper-layer jet slowly meanders and develops a cyclone above the lower-layer eddy. As we increase the jet velocity, the meandering is faster and the cyclone is larger. But a too-strong jet has an opposite effect: the potential vorticity anomalies induced by the lower-layer eddy are quickly swept away, leading to explosive downstream meander growth; no cyclone is formed above the lower-layer eddy. In all cases, the initial meandering trigger is a linear process (the steering of the upper-layer jet by the lower-layer eddy). But even when the upper-layer jet is weak, nonlinearity quickly becomes important, dominating the dynamics after 10 days of simulation. The downstream meander growth is fully nonlinear. Our idealized QG model confirms that the IWBC recirculation can trigger the Vitória Eddy formation and elucidates the mechanisms involved in this process.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1175/BAMS-D-20-0113.1\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021', 'https://doi.org/10.1175/BAMS-D-20-0113.1', event);\">\n    Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Shroyer, E.; Tandon, A.; Sengupta, D.; Fernando, H. J.; Lucas, A. J; Farrar, J T.; Chattopadhyay, R.; de Szoeke, S.; Flatau, M.; Rydbeck, A.;  and others\n</span>\n\n  \n\n</span>\n\n  <i>Bulletin of the American Meteorological Society</i>,1–44.  2021.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1175/BAMS-D-20-0113.1\"\n     onclick=\"log_download('shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021', 'https://doi.org/10.1175/BAMS-D-20-0113.1', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1175/BAMS-D-20-0113.1\"\n     onclick=\"log_download('shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021', 'http://doi.org/10.1175/BAMS-D-20-0113.1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('shroyer-tandon-sengupta-fernando-lucas-farrar-chattopadhyay-deszoeke-etal-bayofbengalintraseasonaloscillationsandthe2018monsoononset-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{shroyer2021bay,\n  title={Bay of Bengal Intraseasonal Oscillations and the 2018 Monsoon Onset},\n  author={Shroyer, Emily and Tandon, Amit and Sengupta, Debasis and Fernando, Harindra JS and Lucas, Andrew J and Farrar, J Thomas and Chattopadhyay, Rajib and de Szoeke, Simon and Flatau, Maria and Rydbeck, Adam and others},\n  journal={Bulletin of the American Meteorological Society},\n  url = {https://doi.org/10.1175/BAMS-D-20-0113.1},\n  doi = {10.1175/BAMS-D-20-0113.1},\n  pages={1--44},\n  year={2021},\n  abstract=&quot;In the Bay of Bengal, the warm, dry boreal spring concludes with the onset of the summer monsoon and accompanying southwesterly winds, heavy rains, and variable air-sea fluxes. Here, we summarize the 2018 monsoon onset using observations collected through the multinational Monsoon Intraseasonal Oscillations in the Bay of Bengal (MISO-BoB) program between the US, India, and Sri Lanka. MISO-BoB aims to improve understanding of monsoon intraseasonal variability, and the 2018 field effort captured the coupled air-sea response during a transition from active-to-break conditions in the central BoB. The active phase of the ~20-day research cruise was characterized by warm sea surface temperature (SST &gt; 30°C), cold atmospheric outflows with intermittent heavy rainfall, and increasing winds (from 2 to 15 m s−1). Accumulated rainfall exceeded 200 mm with 90\\% of precipitation occurring during the first week. The following break period was both dry and clear, with persistent 10−12 m s−1 wind and evaporation of 0.2 mm h−1. The evolving environmental state included a deepening ocean mixed layer (from ~20 to 50 m), cooling SST (by ~ 1°C), and warming/drying of the lower to mid-troposphere. Local atmospheric development was consistent with phasing of the large-scale intraseasonal oscillation. The upper ocean stores significant heat in the BoB, enough to maintain SST above 29°C despite cooling by surface fluxes and ocean mixing. Comparison with reanalysis indicates biases in air-sea fluxes, which may be related to overly cool prescribed SST. Resolution of such biases offers a path toward improved forecasting of transition periods in the monsoon.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  In the Bay of Bengal, the warm, dry boreal spring concludes with the onset of the summer monsoon and accompanying southwesterly winds, heavy rains, and variable air-sea fluxes. Here, we summarize the 2018 monsoon onset using observations collected through the multinational Monsoon Intraseasonal Oscillations in the Bay of Bengal (MISO-BoB) program between the US, India, and Sri Lanka. MISO-BoB aims to improve understanding of monsoon intraseasonal variability, and the 2018 field effort captured the coupled air-sea response during a transition from active-to-break conditions in the central BoB. The active phase of the  20-day research cruise was characterized by warm sea surface temperature (SST > 30°C), cold atmospheric outflows with intermittent heavy rainfall, and increasing winds (from 2 to 15 m s−1). Accumulated rainfall exceeded 200 mm with 90% of precipitation occurring during the first week. The following break period was both dry and clear, with persistent 10−12 m s−1 wind and evaporation of 0.2 mm h−1. The evolving environmental state included a deepening ocean mixed layer (from  20 to 50 m), cooling SST (by   1°C), and warming/drying of the lower to mid-troposphere. Local atmospheric development was consistent with phasing of the large-scale intraseasonal oscillation. The upper ocean stores significant heat in the BoB, enough to maintain SST above 29°C despite cooling by surface fluxes and ocean mixing. Comparison with reanalysis indicates biases in air-sea fluxes, which may be related to overly cool prescribed SST. Resolution of such biases offers a path toward improved forecasting of transition periods in the monsoon.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1029/2021JC017387\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021', 'https://doi.org/10.1029/2021JC017387', event);\">\n    Revisiting the Atlantic South Equatorial Current.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Luko, C.; da Silveira, I.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I.</a>; Araujo, J.;  and Tandon, A\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Geophysical Research: Oceans</i>,e2021JC017387.  2021.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1029/2021JC017387\"\n     onclick=\"log_download('luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021', 'https://doi.org/10.1029/2021JC017387', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Revisiting the Atlantic South Equatorial Current [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1029/2021JC017387\"\n     onclick=\"log_download('luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021', 'http://doi.org/10.1029/2021JC017387', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('luko-dasilveira-simoessousa-araujo-tandon-revisitingtheatlanticsouthequatorialcurrent-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{luko2021revisiting,\n  title={Revisiting the Atlantic South Equatorial Current},\n  author={Luko, CD and da Silveira, ICA and Simoes-Sousa, IT and Araujo, JM and Tandon, A},\n  journal={Journal of Geophysical Research: Oceans},\n  pages={e2021JC017387},\n  url = {https://doi.org/10.1029/2021JC017387},\n  doi = {10.1029/2021JC017387},\n  year={2021},\n  abstract=&quot;The southern branch of the South Equatorial Current (SSEC) is the northern limit of the South Atlantic Subtropical Gyre. When this current reaches Brazil around 14°S it bifurcates into a southward flow as the Brazil Current (BC) and the surface portion of the northward flowing North Brazil Undercurrent (NBUC). The SSEC system is a key component of the western boundary supply, influencing the NBUC/BC variability and, therefore, global climate through the Meridional Overturning Circulation. In this study, using altimetry satellite data and reanalyzes outputs (1993–2018), we revisit the SSEC mean state and show this current arriving at the South Atlantic western boundary as a multi-banded flow with surface signatures resulting from different subsurface cores. These bands have velocities between 0.02 and 0.07 m s$^{−1}$ and, as shown by ADCP data from the PIRATA project, their signature in synoptic scenarios is obscured by eddies and waves with velocities between 0.1 and 0.3 m s$^{−1}$. In addition, the SSEC annual cycle analysis shows that the seasonality of the bands is out of phase with each other, presenting westward transport anomalies between 0.4 and 2.6 Sv. Finally, our results show that the seasonality of this multi-banded flow both defines where the BC is born, and modulates the seasonality of semi-permanent mesoscale eddies off Brazil.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The southern branch of the South Equatorial Current (SSEC) is the northern limit of the South Atlantic Subtropical Gyre. When this current reaches Brazil around 14°S it bifurcates into a southward flow as the Brazil Current (BC) and the surface portion of the northward flowing North Brazil Undercurrent (NBUC). The SSEC system is a key component of the western boundary supply, influencing the NBUC/BC variability and, therefore, global climate through the Meridional Overturning Circulation. In this study, using altimetry satellite data and reanalyzes outputs (1993–2018), we revisit the SSEC mean state and show this current arriving at the South Atlantic western boundary as a multi-banded flow with surface signatures resulting from different subsurface cores. These bands have velocities between 0.02 and 0.07 m s$^{−1}$ and, as shown by ADCP data from the PIRATA project, their signature in synoptic scenarios is obscured by eddies and waves with velocities between 0.1 and 0.3 m s$^{−1}$. In addition, the SSEC annual cycle analysis shows that the seasonality of the bands is out of phase with each other, presenting westward transport anomalies between 0.4 and 2.6 Sv. Finally, our results show that the seasonality of this multi-banded flow both defines where the BC is born, and modulates the seasonality of semi-permanent mesoscale eddies off Brazil.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1590/2675-2824069.20-011psp\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021', 'https://doi.org/10.1590/2675-2824069.20-011psp', event);\">\n    Insights on the non-linear solution of Munk's ocean circulation theory from a rotating tank experiment.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Polito, P. S.; Sato, O. T.; Napolitano, D. C.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T.</a>; Almeida, H.;  and Lapolli, F. R.\n</span>\n\n  \n\n</span>\n\n  <i>Ocean and Coastal Research</i>, 69.  2021.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1590/2675-2824069.20-011psp\"\n     onclick=\"log_download('polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021', 'https://doi.org/10.1590/2675-2824069.20-011psp', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Insights on the non-linear solution of Munk&#x27;s ocean circulation theory from a rotating tank experiment [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1590/2675-2824069.20-011psp\"\n     onclick=\"log_download('polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021', 'http://doi.org/10.1590/2675-2824069.20-011psp', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('polito-sato-napolitano-simoessousa-almeida-lapolli-insightsonthenonlinearsolutionofmunksoceancirculationtheoryfromarotatingtankexperiment-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{polito2021,\n  title = {Insights on the non-linear solution of Munk&#x27;s ocean circulation theory from a rotating tank experiment},\n  author = {Paulo S. Polito and Olga T. Sato and Dante C. Napolitano and Iury T. Simoes-Sousa and Helio Almeida and Fabricio R. Lapolli},\n  journal = {Ocean and Coastal Research},\n  doi = {10.1590/2675-2824069.20-011psp},\n  url = {https://doi.org/10.1590/2675-2824069.20-011psp},\n  year = {2021},\n  publisher = {{FapUNIFESP} ({SciELO})},\n  volume = {69},\n  abstract = &quot;At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk&#x27;s circulation theory aided by a Lagrangian particles tracking algorithm and numerical modeling. From information captured by video, we track the trajectories of drifters, and then objectively mapped the streamfunction to obtain the mean circulation pattern. We were able to reproduce the wind-forced anticyclonic and asymmetric gyre, including the western boundary intensification and its retroflection. The latter phenomenon was predicted by the non-linear version of Munk&#x27;s model and observed in real subtropical gyres as small recirculation regions. We have configured two numerical model simulations mimicking the physical experiment, with linear and non-linear terms. The comparison between the numerical and physical experiments confirmed the effect of non-linear distortion of the gyre. Geophysical fluid dynamics is often hard to visualize, and counter-intuitive in a rotating system. We present this set of experiments as a tool for oceanography teaching. Besides studying general ocean circulation theories and observations through practical examples, this experiment provides an opportunity to develop basic image processing and geophysical modelling skills.&quot;,\n}\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  At age 101, Walter Munk passed away in 2019. His groundbreaking discoveries will still guide and amaze oceanography students for years to come. Here, we perceive patterns in rotating tank with Munk's circulation theory aided by a Lagrangian particles tracking algorithm and numerical modeling. From information captured by video, we track the trajectories of drifters, and then objectively mapped the streamfunction to obtain the mean circulation pattern. We were able to reproduce the wind-forced anticyclonic and asymmetric gyre, including the western boundary intensification and its retroflection. The latter phenomenon was predicted by the non-linear version of Munk's model and observed in real subtropical gyres as small recirculation regions. We have configured two numerical model simulations mimicking the physical experiment, with linear and non-linear terms. The comparison between the numerical and physical experiments confirmed the effect of non-linear distortion of the gyre. Geophysical fluid dynamics is often hard to visualize, and counter-intuitive in a rotating system. We present this set of experiments as a tool for oceanography teaching. Besides studying general ocean circulation theories and observations through practical examples, this experiment provides an opportunity to develop basic image processing and geophysical modelling skills.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2019\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2019')\"\n      onkeypress=\"toggleGroup('group_2019')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2019</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.2174/1871520619666190207130732\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019', 'https://doi.org/10.2174/1871520619666190207130732', event);\">\n    Biological and Toxicological Evaluation of N-(4methyl-phenyl)-4-methylphthalimide on Bone Cancer in Mice.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Santin, J. R; da Silva, G. F; Pastor, M. V.; Broering, M. F; Nunes, R.; Braga, R. C; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I. T.</a>; Stiz, D. S; da Silva, K. A.; Stoeberl, L. C;  and others\n</span>\n\n  \n\n</span>\n\n  <i>Anti-Cancer Agents in Medicinal Chemistry (Formerly Current Medicinal Chemistry-Anti-Cancer Agents)</i>, 19(5): 667–676.  2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.2174/1871520619666190207130732\"\n     onclick=\"log_download('santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019', 'https://doi.org/10.2174/1871520619666190207130732', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Biological and Toxicological Evaluation of N-(4methyl-phenyl)-4-methylphthalimide on Bone Cancer in Mice [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.2174/1871520619666190207130732\"\n     onclick=\"log_download('santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019', 'http://doi.org/10.2174/1871520619666190207130732', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('santin-dasilva-pastor-broering-nunes-braga-simoessousa-stiz-etal-biologicalandtoxicologicalevaluationofn4methylphenyl4methylphthalimideonbonecancerinmice-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{santin2019biological,\n  title={Biological and Toxicological Evaluation of N-(4methyl-phenyl)-4-methylphthalimide on Bone Cancer in Mice},\n  author={Santin, Jose R and da Silva, Gislaine F and Pastor, Maria VD and Broering, Milena F and Nunes, Roberta and Braga, Rodolpho C and Simoes-Sousa, Iury T. and Stiz, Dorimar S and da Silva, Kathryn ABS and Stoeberl, Luis C and others},\n  journal={Anti-Cancer Agents in Medicinal Chemistry (Formerly Current Medicinal Chemistry-Anti-Cancer Agents)},\n  url = {https://doi.org/10.2174/1871520619666190207130732},\n  doi = {10.2174/1871520619666190207130732},\n  volume={19},\n  number={5},\n  pages={667--676},\n  year={2019},\n  publisher={Bentham Science Publishers}\n}\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2018\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2018')\"\n      onkeypress=\"toggleGroup('group_2018')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2018</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"silveira-napolitano-simoessousa-parkinson-watanabe-ascorrentesocenicasnabaciasergipealagoas-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'silveira-napolitano-simoessousa-parkinson-watanabe-ascorrentesocenicasnabaciasergipealagoas-2018', 'https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/', event);\">\n    As Correntes Oceânicas na Bacia Sergipe-Alagoas.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Silveira, I.; Napolitano, D.; <a class=\"bibbase author link\" href=\"https://iuryt.github.io/publications.html\">Simoes-Sousa, I.</a>; Parkinson, R.;  and Watanabe, W.\n</span>\n\n  \n\n</span>\n\n  <i>Revista Marseal: Edição Águas Profundas SE/AL</i>, 2: 36–39.  2018.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/\"\n     onclick=\"log_download('silveira-napolitano-simoessousa-parkinson-watanabe-ascorrentesocenicasnabaciasergipealagoas-2018', 'https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"As Correntes Oceânicas na Bacia Sergipe-Alagoas [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/silveira-napolitano-simoessousa-parkinson-watanabe-ascorrentesocenicasnabaciasergipealagoas-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('silveira-napolitano-simoessousa-parkinson-watanabe-ascorrentesocenicasnabaciasergipealagoas-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{marseal2018,\n  title = {As Correntes Oceânicas na {Bacia Sergipe-Alagoas}},\n  author = {Ilson Silveira and Dante Napolitano and Iury Simoes-Sousa and Renato Parkinson and Wandrey Watanabe},\n  journal = {Revista Marseal: Edição Águas Profundas SE/AL},\n  year = {2018},\n  volume = {2},\n  pages = {36--39},\n  issn = {2596-0547},\n  publisher = {Editora UFS e Centro de Pesquisas da Petrobras (CENPES)},\n  url = {https://www.livraria.ufs.br/produto/revista-marseal-edicao-aguas-profundas-seal-volume-2/}\n}\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n\n\n\n  </div>\n\n\n  <!-- Modal -->\n\n  <!-- <iframe id=\"bibbase_network_frame\" -->\n  <!--         src=\"//bibbase.org/network/control\" -->\n  <!--         style=\"display: none;\"> -->\n  <!-- </iframe> -->\n\n</div>\n"}; 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