Leonardo de Souza Bruno

Mr. Leonardo de Souza Bruno


Research Focus & Metrics

Academic Career Length

5Years (2022-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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9 December 2022 in Hydrology
Verified
Journal Article
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LBLeonardo de Souza Bruno
Leonardo de Souza Bruno
TMTiago Souza Mattos
Tiago Souza Mattos
POPaulo Tarso S. Oliveira
Paulo Tarso S. Oliveira
AAAndre Almagro
Andre Almagro
DRDulce Buchala Bicca Rodrigues
Dulce Buchala Bicca Rodrigues
In flood area mapping studies, hydrological-hydraulic modeling has been successfully applied around the world. However, the object of study of most of the research developed in Brazil is medium to large channels that use topographical and hydrometeorological data of coarse spatial and temporal resolution. Thus, the aim of this study is to investigate coupled modeling in a small urban channel, using high-resolution data, in the simulation of flood events in a small urban channel, located in Campo Grande, Mato Grosso do Sul. In this study, we used the HEC-HMS and HEC-RAS programs, where topographic information, land use, land cover, and observed data from rain gauges, water level, and flow sensors from 2015 to 2018 were used as input data. To calibrate and validate the hydrological model, four events were used that occurred during the monitoring period, while in the hydraulic model we chose a historical event that caused great disturbances. We then generated flood scenarios with representative synthetic rainfall for a basin, with return times of 5, 10, 50, and 100 years. We observed a good fit in the calibration and validation of the HEC-HMS, with values of R2 = 0.93, RMSE = 1.29, and NSE = 0.92. In HEC-RAS, we obtained values of R2 = 0.93, RMSE = 1.29, and NSE = 0.92 for the calibration, and in the validation, real images of the event prove the computed flood spot sources. We observed that rain with a return time of less than five years provides areas of flooding in several regions of the channel, and in critical channeled sections, the elevation and speed of the flow reach 5 m and 3 m·s−1, respectively. Our results indicate that the channel already has a natural tendency towards flooding in certain stretches, which become more compromised due to land use and coverage and local conditions. We conclude that the high-resolution coupled modeling generated information that represents local conditions as well, showing how potential failures of drainage in extreme scenarios are possible, thus enabling the planning of adaptations and protection measures against floods.

4 March 2022 in Environmental Modelling & Software
Verified
Journal Article
Closed access
TMTiago Mattos
Tiago Mattos
POPaulo Tarso S. Oliveira
Paulo Tarso S. Oliveira
LBLeonardo de Souza Bruno
Leonardo de Souza Bruno
GCGlauber Glauber Altrao altrão carvalho
Glauber Glauber Altrao altrão carvalho
RPRodrigo Pereira
Rodrigo Pereira
TRTirthankar Roy
Tirthankar Roy