2022
DOI: 10.1007/s00348-021-03369-3
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Assimilation and extension of particle image velocimetry data of turbulent Rayleigh–Bénard convection using direct numerical simulations

Abstract: A novel method for assimilating and extending measured turbulent Rayleigh–Bénard convection data is presented, which relies on the fractional step method also used to solve the incompressible Navier–Stokes equation in direct numerical simulations. Our approach is used to make measured tomographic particle image velocimetry (tomo PIV) fields divergence-free and to extract temperature fields. Comparing the time average of the extracted temperature fields with the temporally averaged temperature field, measured u… Show more

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Cited by 4 publications
(2 citation statements)
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“…imaging (Bauer et al, 2022). In fact, forward numerical simulations to calculate the transport of chemical species in turbulent flows usually do not consider identical particles, but define the number density per unit cell, which is solved by using an advection-diffusion equation (e.g., volcanic ash in a pyroclastic flow; Shimizu et al, 2019).…”
Section: Application To Fluids Containing Traceable Particlesmentioning
confidence: 99%
See 1 more Smart Citation
“…imaging (Bauer et al, 2022). In fact, forward numerical simulations to calculate the transport of chemical species in turbulent flows usually do not consider identical particles, but define the number density per unit cell, which is solved by using an advection-diffusion equation (e.g., volcanic ash in a pyroclastic flow; Shimizu et al, 2019).…”
Section: Application To Fluids Containing Traceable Particlesmentioning
confidence: 99%
“…Although some studies include Lagrangian particles in 4D-Var, their scheme does not use any "Lagrangian" information to constrain thermal and flow processes, but the path of Lagrangian particles is estimated based on the velocity fields optimized by Eulerian observations (Ghelichkhan et al, 2021;Nakao et al, 2024). Some studies in fluid dynamical communities use Lagrangian information to reconstruct Rayleigh-Bénard convection by using a sequential data assimilation (Bauer et al, 2022), but to our knowledge, a 4D-Var scheme that considers markers and grids in a system is very rare even in communities outside geodynamics. Thus, there are probably no previous studies that use Lagrangian information to estimate their origin or the time evolution of the surrounding Eulerian field.…”
Section: Introductionmentioning
confidence: 99%