Saulo Meirelles

ORCID: 0000-0003-1257-0708
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About
Contact & Profiles
Research Areas
  • Coastal and Marine Dynamics
  • Geological formations and processes
  • Coastal wetland ecosystem dynamics
  • Coastal and Marine Management
  • Aeolian processes and effects
  • Ocean Waves and Remote Sensing
  • Maritime Ports and Logistics
  • Fluid Dynamics Simulations and Interactions
  • Oceanographic and Atmospheric Processes
  • Geology and Paleoclimatology Research
  • Tropical and Extratropical Cyclones Research
  • Aquatic and Environmental Studies
  • Geological Modeling and Analysis

Delft University of Technology
2014-2024

Statistics New Zealand
2024

Universidade do Estado do Rio de Janeiro
2007-2008

Abstract Wave‐supported gravity flows (WSGFs) generate rates of sediment flux far exceeding other cross‐shelf transport processes, contributing disproportionately to shelf morphology and net fluxes in many regions worldwide. However, the conditions deemed necessary for formation WSGF limit them a narrow set conditions; they have been observed exclusively where seabed consists very fine‐grained typically co‐occur with nearby river flood events. Here we document occurrence event on...

10.1029/2018gl077936 article EN publisher-specific-oa Geophysical Research Letters 2018-07-06

Abstract We present a new mechanism for cross‐shore transport of fine sediment from the nearshore to inner shelf resulting onshore propagation river plume fronts. Onshore frontal is observed in moorings and radar images, which show that fronts penetrate through surf zone, almost waterline. During passage two‐layer counterrotating velocity field characteristic tidal straining immediately set up, generating net offshore flow beneath plume. The seaward at depth carries with it high suspended...

10.1002/2017gl073378 article EN Geophysical Research Letters 2017-05-09

We present direct measurements of seafloor ripple dimensions, near-bed mean flow Reynolds stresses and turbulent sediment fluxes on a sandy inner shelf subjected to strong wave tidal current forcing. The dimensions (height, wavelength) are used evaluate the performance methodology for incorporation non-equilibrium dynamics into calculations drag exerted by bed overlying (i.e., stress) using boundary layer model wave–current interaction. is based simultaneous use existing models...

10.3390/jmse12122116 article EN cc-by Journal of Marine Science and Engineering 2024-11-21

10.1016/j.margeo.2016.03.006 article EN publisher-specific-oa Marine Geology 2016-03-26

Meirelles, S.; Henriquez, M.; Souza, A.J.; Horner-Devine, A.R.; Pietrzak, J.D.; Rijnsburg, S., and Stive, M.J.F., 2016. Small scale bedform types off the South Holland coast. In: Vila-Concejo, A.; Bruce, E.; Kennedy, D.M., McCarroll, R.J. (eds.), Proceedings of 14th International Coastal Symposium (Sydney, Australia). Journal Research, Special Issue, No. 75, pp. 423–426. Coconut Creek (Florida), ISSN 0749-0208.This study presents small states found South-Holland coast during a 31 days field...

10.2112/si75-085.1 article EN Journal of Coastal Research 2016-03-03

Este artigo discute como as transformações sofridas pelas ondas aquáticas ao se aproximarem de águas rasas podem auxiliar o entendimento dos principais fenômenos estudados na óptica. A partir alguns conceitos comuns a todos os ondulatórios, é possível conhecer comportamento das superfície corpos d'água conforme elas encaminham para menores profundidades, que aproximam uma praia. Tornou-se possível, dessa forma, traçar um paralelo entre luminosas e aquáticas. modelagem computacional...

10.1590/s1806-11172007000400014 article PT cc-by Revista Brasileira de Ensino de Física 2007-01-01

O modelo de geração e propagação ondas SWAN é amplamente utilizado pela comunidade científica para obtenção estimativas do espectro em áreas costeiras, lagos estuários. cálculo da difração não era representado no tornando as simulações regiões próximas a obstáculos ou portos menos precisas. Recentemente, uma aproximação o foi implementada, porém poucos trabalhos publicados até momento abordam esta questão. Seu desempenho então investigado um terminal portuário, região onde reflexão são...

10.1590/s0102-261x2008000100004 article PT Brazilian Journal of Geophysics 2008-03-01

Meirelles, S., Horner-Devine, A.R., Henriquez, M., Stive, Pietrzak, J., Souza, A.J., 2014. Middle shoreface sand transport under stratified regimes. In: Green, A.N. and Cooper, J.A.G. (eds.), Proceedings 13th International Coastal Symposium (Durban, South Africa), Journal of Research, Special Issue No. 70, pp. 182–186, ISSN 0749-0208.Observations from a field experiment along the south-Holland coast, Netherlands, were carried out in order to obtain new insights about impacts Rhine ROFI...

10.2112/si70-031.1 article EN Journal of Coastal Research 2014-04-28

The South-Holland coast of the Netherlands undergoes influence Rhine river plume released from Rotterdam waterways. An experiment, STRAINS, was conducted to study impact fresh water on nearshore hydrodynamics and sand transport. As part an instrumented bottom frame measured near-bed at 12 m depth. flow decomposed in tidal, wave turbulent component. During moderate energetic conditions cross-shore tidal similar magnitude as orbital flow. asymmetric larger seaward direction. component may be...

10.9753/icce.v34.currents.33 article EN cc-by Coastal Engineering Proceedings 2014-10-30

Este artigo discute como as transformações sofridas pelas ondas aquáticas ao se aproximarem de águas rasas podem auxiliar o entendimento dos principais fenômenos estudados na óptica. A partir alguns conceitos comuns a todos os ondulatórios, é possível conhecer comportamento das superfície corpos d'água conforme elas encaminham para menores profundidades, que aproximam uma praia. Tornou-se possível, dessa forma, traçar um paralelo entre luminosas e aquáticas. modelagem computacional...

10.1590/s0102-47442007000400014 article PT Revista de ensino de física 2007-01-01

This thesis examines the effects of stratified tidal flow on morphodynamics Dutch inner shelf. The south portion shelf is strongly influenced by Rhine River ROFI (Region Of Freshwater Influence), which generated discharge from through Rotterdam waterways. Under conditions, three-dimensional structure currents develops a strong cross-shore shear so that bottom and surface become 180deg out phase. sheared created stratification operates in nearshore zones asymmetries imparted are expected to...

10.4233/uuid:b98e7799-c0d3-42ca-8c9c-70ee64bf059a article EN 2019-01-07
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