Current Organizations / Institutes

The organizations/institutes from the scholar's latest article

Previous Organizations / Institutes

The organizations / institutes from the scholar's other articles in the past ten years


Ricardo de Camargo has a total of 158 co-authors. Here are the top co-authors by number of shared publications:


Latest Publications

  • Open Access

    Compound coastal risk from waves and sea level along the Brazilian coast

    by Danilo Couto de Souza, Karine Bastos Leal, Carolina Barnez Gramcianinov, Ricardo de Camargo

  • Open Access

    Addressing the large-sample-size effect in wind-speed goodness-of-fit through temporal segmentation and Monte-Carlo simulation

    by Danilo Couto de Souza, Luis Manoel Paiva Nunes, Ricardo de Camargo, Felipe Mendonça Pimenta, Marcelo Andrioni, Eric O. Ribeiro

  • Open Access

    A vessel-mounted continuous-wave Lidar system for offshore wind surveys

    by Felipe M. Pimenta, Osvaldo R. Saavedra, Ricardo de Camargo, Allan R. Silva, Arcilan T. Assireu, Denivaldo C.P. Lopes, Shigeaki L. de Lima, Danilo Couto de Souza, Luis Manoel P. Nunes, Marcelo Andrioni

  • Open Access

    Revisiting the rare transition of a South Atlantic cyclone to tropical storm Akará: energy cycle and stratosphere-troposphere interaction

    by de Souza, Danilo Couto, Victor Antunes Ranieri, Silva Dias, Pedro Leite da, Andres Rodríguez Flores, Ricardo Camargo

    Cyclone Akará was the third documented tropical cyclone in the South Atlantic, undergoing a rare subtropical-to-tropical transition in February 2024. This study investigates the dynamical, thermodynamical, and energetic evolution of Akará using a diagnostic framework combining the Lorenz Energy Cycle (LEC) and heat and vorticity budgets. Akará originated in a post-frontal, weakly baroclinic environment characterized by warm sea surface temperatures ( $$>28^{\circ } C$$ ), strong ocean–atmosphere thermal contrast, and low vertical wind shear. These conditions favored convective activity and led to the development of a symmetric warm core, initially supported by latent heat release and interaction with an upper-level cutoff low. As the system intensified, it transitioned into a tropical cyclone, exhibiting a deep warm core and organized convection. Stratospheric air intrusions were identified during and after the tropical transition, contributing to upper-tropospheric warming and enhancing cyclone intensification. Heat and vorticity budget analyses revealed how vertical motion, latent heat release, and vortex stretching shaped the storm’s three-dimensional structure and contributed to its deepening. During the mature stage, Akará reached peak intensity while moving over cooler waters. Although convective activity decreased, the warm core was sustained-likely through continued stratosphere-troposphere interactions and strong barotropic energy conversions at low and mid levels. The combined use of LEC and budget diagnostics proved effective in disentangling the physical mechanisms behind Akará’s evolution, offering valuable insight into the dynamics of rare South Atlantic tropical transitions. Expanding such analyses to other events is essential to improve our understanding and forecasting of tropical cyclogenesis in this basin.


  • Open Access

    Addressing the Large-Sample-Size Effect in Wind-Speed Goodness-of-Fit through Temporal Segmentation and Monte-Carlo Simulation

    by Danilo Couto de Souza, Luis Manoel Paiva Nunes, Ricardo de Camargo, Felipe Pimenta, Eric Oliveira Ribeiro, Marcelo Andrioni

    Reliable wind-resource assessment hinges on a robust statistical description of the wind-speed frequency distribution, often obtained via a two-parameter Weibull fit. International guidelines routinely require that such fits be accompanied by formal goodness-of-fit (GoF) tests, with acceptance based on p-value thresholds. However, for modern multi-year, high-frequency records, GoF tests become overly sensitive and p-values collapse toward zero, leading to rejections of otherwise satisfactory fits — even though larger samples should, in principle, yield more reliable parameter estimates. This apparent paradox is known as the large-sample-size effect and can bias practical decisions on model adequacy and complexity. Here, we propose an objective framework to mitigate this effect by combining Monte Carlo (MC) subsampling with temporal segmentation. The MC procedure draws repeated subsamples from the original record, fits the target parametric distribution, and evaluates each fit using the $\chi^{2}$ and Kolmogorov--Smirnov (KS) tests and the root-mean-square error (RMSE). While GoF-test p-values systematically decrease with increasing sample size, RMSE stabilizes beyond a characteristic threshold. We detect this stabilization point to define an optimal effective sample size, from which statistically supported parameters are recommended for subsequent use. We apply the method to reanalysis winds and in situ meteorological observations (INMET). Across ERA5 and INMET records, full-sample Weibull fits frequently failed $\chi^{2}$/KS due to inflated test power, whereas temporal segmentation combined with RMSE-stability subsampling restored statistically interpretable p-values and increased “pass-both” rates from $\sim$25\% to $\sim$76\% on average across stations, without distorting the inferred diurnal and seasonal structure of $(k,c)$. Temporal segmentation further indicates that fitted parameters are not intrinsic site constants, but emergent summaries of superimposed weather regimes, with diurnal--seasonal variability in $(k,c)$ reflecting shifts in the relative dominance of distinct atmospheric circulation patterns. Overall, the proposed framework mitigates large-sample-size artefacts while preserving physically meaningful variability, providing a practical, standards-compatible route for reporting parametric wind-speed statistics from modern high-frequency records. Although demonstrated with the Weibull law, the approach is readily transferable to any desired parametric distribution and helps distinguish genuinely non-conforming regimes from purely sample-size-driven rejections.

  • Open Access

    Ocean dynamics in 2025: overview and thank you to reviewers

    by Tal Ezer, Antonio Bonaduce, Diego Bruciaferri, Sandro Carniel, Amin Chabchoub, W. Bryce Corlett, Ricardo de Camargo, Sheila N. Estrada-Allis, Oliver B. Fringer, Avijit Gangopadhyay, et al.

  • Lorenz Energy Cycle Climatology for the Southwestern Atlantic Cyclones

    by de Souza, Danilo Couto, Silva Dias, Pedro Leite da, Carolina Barnez Gramcianinov, Ricardo Camargo


  • Open Access

    Lorenz Energy Cycle Climatology for the Southwestern Atlantic Cyclones

    by Danilo Couto de Souza, Pedro Leite da Silva Dias, Carolina Barnez Gramcianinov, Ricardo Camargo

    This study presents a climatological assessment of the Lorenz Energy Cycle (LEC) applied to South Atlantic cyclones, using a Semi-Lagrangian framework. Over 6,700 cyclones were identified from ERA5 reanalysis (1979–2020), and LEC components were computed and averaged across four objectively defined life cycle phases: incipient, intensification, mature, and decay. Results reveal a coherent energy transfer structure: baroclinic conversions dominate during intensification, while barotropic conversions peak during the mature phase and reach magnitudes 2–3 times larger than baroclinic counterparts. Diabatic generation of eddy available potential energy plays a secondary but relevant role, particularly during intensification, occasionally surpassing baroclinic contributions. Eddy kinetic energy imports are most significant during the early phases, reinforcing development. Despite substantial variability among systems, an EOF analysis shows that most cyclones share a common energy structure, with variability manifesting as amplification or suppression of specific pathways. The leading EOFs are linked to differences in cyclone intensity, genesis region, and seasonality. Among the most intense systems, distinct clusters emerge with varying energetic configurations, some dominated by baroclinic processes, others by barotropic conversions or enhanced diabatic generation. These findings demonstrate that South Atlantic cyclones encompass a spectrum of dynamical behaviors and can be classified based on their energy cycle characteristics. This study provides the first large-sample application of the Semi-Lagrangian LEC to extratropical cyclones in the South Atlantic and highlights the importance of barotropic processes in their development. The results offer a robust framework for interpreting cyclone energetics and establish a comprehensive baseline for classifying these systems.

  • Open Access

    Revisiting The Rare Transition of a South Atlantic Cyclone to Tropical Storm Akará: Energy Cycle and Stratosphere-Troposphere Interaction

    by Danilo Couto de Souza, Victor Antunes Ranieri, Pedro Leite da Silva Dias, Andres Rodríguez Flores, Ricardo de Camargo

    Cyclone Akará was the third documented tropical cyclone in the South Atlantic, undergoing a rare subtropical-to-tropical transition in February 2024. This study investigates the dynamical, thermodynamical, and energetic evolution of Akará using a diagnostic framework combining the Lorenz Energy Cycle (LEC) and heat and vorticity budgets. Akará originated in a post-frontal, weakly baroclinic environment characterized by warm sea surface temperatures (>28$\circ C$), strong ocean-atmosphere thermal contrast, and low vertical wind shear. These conditions favored convective activity and led to the development of a symmetric warm core, initially supported by latent heat release and interaction with an upper-level cutoff low. As the system intensified, it transitioned into a tropical cyclone, exhibiting a deep warm core and organized convection. Stratospheric air intrusions were identified during and after the tropical transition, contributing to upper-tropospheric warming and enhancing cyclone intensification. Heat and vorticity budget analyses revealed how vertical motion, latent heat release, and vortex stretching shaped the storm’s three-dimensional structure and contributed to its deepening. During the mature stage, Akará reached peak intensity while moving over cooler waters. Although convective activity decreased, the warm core was sustained—likely through continued stratosphere-troposphere interactions and strong barotropic energy conversions at low and mid levels. The combined use of LEC and budget diagnostics proved effective in disentangling the physical mechanisms behind Akará's evolution, offering valuable insight into the dynamics of rare South Atlantic tropical transitions. Expanding such analyses to other events is essential to improve our understanding and forecasting of tropical cyclogenesis in this basin.


  • Open Access

    CycloPhaser: A Python Package for Detecting Extratropical Cyclone Life Cycles

    by Danilo Couto de Souza, Pedro Leite da Silva Dias, Carolina Barnez Gramcianinov, Ricardo de Camargo

    CycloPhaser is a Python package designed to detect and analyze extratropical cyclone life cycles from central relative vorticity data. It enables researchers in meteorology and atmospheric sciences to automatically identify key stages of cyclone development, such as intensification, decay, and mature phases, using the vorticity series and its derivatives. By leveraging vorticity data, CycloPhaser helps scientists study cyclones across various regions and timeframes, contributing to improved understanding of cyclone energetics and behavior.