Ugo Piomelli
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About
Ugo Piomelli is a Professor at Queen's University, Canada. His research focuses on turbulence and fluid dynamics, particularly in large-eddy simulations and the behavior of turbulent boundary layers. Recent publications include investigations into wall-modelled simulations, unsteady separation in turbulent flow, and the effects of surface roughness on scalar transport.
Recent Grants
Grant: Close
Numerical simulation and modelling of non-equilibrium flows in hydro-power applications
Open Date: 2017-04-01
Close Date: 2018-03-31
Grant: Close
Turbulence Simulations and Modelling
Open Date: 2017-04-01
Close Date: 2018-03-31
Grant: Close
Turbulence Simulations and Modelling
Open Date: 2016-04-01
Close Date: 2017-03-31
Grant: Close
Large-eddy simulations of complex turbulent flows
Open Date: 2016-04-01
Close Date: 2018-03-31
Grant: Close
Canada Research Chair in Computational Turbulence
Open Date: 2015-04-01
Close Date: 2016-03-31
Articles (10)
Year:
2026
Year:
2025
Year:
2025
Unsteady separation is a phenomenon that occurs in many flows and results in increased drag, decreased lift, noise emission, and loss of efficiency or failure in flow devices. Turbulence models for the steady or unsteady Reynolds-averaged Navier–Stokes equations (RANS and URANS, respectively) are commonly used in industry; however, their performance is often unsatisfactory. The comparison of RANS results with experimental data does not clearly isolate the modeling errors, since differences with the data may be due to a combination of modeling and numerical errors, and also to possible differences in the boundary conditions. In the present study, we use high-fidelity large-eddy simulation (LES) results to carry out a consistent evaluation of the turbulence models. By using the same numerical scheme and boundary conditions as the LES, and a grid on which grid convergence was achieved, we can isolate modeling errors. The calculations (both LES and RANS) are carried out using a well-validated, second-order-accurate code. Separation is generated by imposing a freestream velocity distribution, that is modulated in time. We examined three frequencies (a rapid, flutter-like oscillation, an intermediate one in which the forcing and the flow have the same timescales, and a quasi-steady one). We also considered three different pressure distributions, one with alternating favorable and adverse pressure gradients (FPGs and APGs, respectively), one oscillating between an APG and a zero-pressure gradient (ZPG), and one with an oscillating APG. All turbulence models capture the general features of this complex unsteady flow as well or better than in similar steady cases. The presence, during the cycle, of times in which the freestream pressure-gradient is close to zero affects significantly the model performance. Comparing our results with those in the literature indicates that numerical errors due to the type of discretization and the grid resolution are as significant as those due to the turbulence model.
Year:
2023
Year:
2023
Year:
2022
Year:
2022
Year:
2022
Year:
2021
Year:
2020
Collaborators (3)
Giuliano De Stefano
Associate Professor
Università degli Studi della Campania Luigi Vanvitelli
David Rival
Associate Professor
Queen's University
Francesco Ambrogi
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