Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Marcos Nicolás Gallo"'
Autor:
Layrson de Jesus Menezes Gonçalves, Júlia Kaiser, Ronaldo Maia de Jesus Palmeira, Marcos Nicolás Gallo, Carlos Eduardo Parente
Publikováno v:
Atmosphere, Vol 15, Iss 5, p 533 (2024)
This study assesses the performance of the Weather Research and Forecasting (WRF) model using a high-resolution spatial grid (1 km) with various combinations of physical parameterization packages to simulate a severe event in August 2021 in the south
Externí odkaz:
https://doaj.org/article/045fd3d10217412e94397b80b8dc2e30
Autor:
Nair Emmanuela da Silveira Pereira, Susana Beatriz Vinzón, Marcos Nicolás Gallo, Mariela Gabioux
Publikováno v:
Hydrology, Vol 11, Iss 2, p 15 (2024)
On the southeastern coast of Brazil, the bays of Ilha Grande and Sepetiba are linked by the Ilha Grande Channel, where remarkably strong currents have been consistently observed. Tidal forces cannot explain the strength of these currents. Previous re
Externí odkaz:
https://doaj.org/article/0961e13ac87348328b3fc80dbe3dc706
Publikováno v:
Water, Vol 11, Iss 2, p 340 (2019)
To develop beach engineering, the submerged structure’s primary physical functions have to be understood. This study focuses on submerged structures in order to understand the strategy of reduced wave energy, stabilizing the shoreline and not gener
Externí odkaz:
https://doaj.org/article/1153892d8a4e496eabcfbae2fd4979de
Publikováno v:
Ocean Dynamics. 70:573-590
Many ports and navigation channels around the world suffer from silting and the presence of fluid mud layers, which can cause reductions in nautical depth. In this context, the existence of fluid mud layers makes the definition of the bottom ambiguou
Autor:
Susana B. Vinzon, Diego Luiz Fonseca, Juliane Castro Carneiro, Patricia da Cunha Marroig, Marcos Nicolás Gallo
Publikováno v:
Ocean Dynamics. 69:51-57
At the nautical bottom approach, part of the fluid mud layers can be included in the available depth if they present favorable rheology. As it is difficult to perform in situ rheological profiles, the most adopted procedure is to correlate these prop
Publikováno v:
Geomorphology. 308:107-117
The distortion of the tide in estuaries, bays and coastal areas is the result of the generation of overtides due to the non-linear effects associated with friction, advection, and the finite effects of the tidal amplitude in shallow waters. The Beira
Publikováno v:
Revista de Gestão Costeira Integrada. 18:49-69
Publikováno v:
Journal of South American Earth Sciences. 112:103603
Estuaries often have interconnected pathways, which may result in complex tidal dynamics that create a tidal meeting point inside the channels. Consequently, channels near urban centers could experience siltation and pollution problems due to intense
Autor:
Boris Ávila, Marcos Nicolás Gallo
Publikováno v:
Journal of South American Earth Sciences. 108:103215
Morphological conditions of river deltas define the sedimentological processes of this kind of ecosystem, which are strategic points to locate transport infrastructures, such as ports. River deltas can present morphological variations caused by natur
Publikováno v:
Continental Shelf Research. 148:37-43
The ability to predict the sediment and nutrient circulation within estuarine waters is of significant economic and ecological importance. In these complex systems, flocculation is a dynamically active process that is directly affected by the prevale