On the Convergence and Capability of the Large-Eddy Simulation of Concentration Fluctuations in Passive Plumes for a Neutral Boundary Layer at Infinite Reynolds Number.

Concentration moments Large-eddy simulation grid resolution Plume dispersion Probability density function Turbulence

Journal

Boundary-layer meteorology
ISSN: 0006-8314
Titre abrégé: Boundary Layer Meteorol
Pays: Netherlands
ID NLM: 101622294

Informations de publication

Date de publication:
2020
Historique:
received: 09 10 2019
accepted: 26 05 2020
entrez: 18 8 2020
pubmed: 18 8 2020
medline: 18 8 2020
Statut: ppublish

Résumé

Large-eddy simulation (LES) experiments have been performed using the Parallelized LES Model (PALM). A methodology for validating and understanding LES results for plume dispersion and concentration fluctuations in an atmospheric-like flow is presented. A wide range of grid resolutions is shown to be necessary for investigating the convergence of statistical characteristics of velocity and scalar fields. For the scalar, the statistical moments up to the fourth order and the shape of the concentration probability density function (p.d.f.) are examined. The mean concentration is influenced by grid resolution, with the highest resolution simulation showing a lower mean concentration, linked to larger turbulent structures. However, a clear tendency to convergence of the concentration variance is observed at the two higher resolutions. This behaviour is explained by showing that the mechanisms driving the mean and the variance are differently influenced by the grid resolution. The analysis of skewness and kurtosis allows also the obtaining of general results on plume concentration fluctuations. Irrespective of grid resolution, a family of Gamma p.d.f.s well represents the shape of the concentration p.d.f. but only beyond the peak of the concentration fluctuation intensity. In the early plume dispersion phases, the moments of the p.d.f. are in good agreement with those generated by a fluctuating plume model. To the best of our knowledge, our study demonstrates for the first time that, if resolution and averaging time are adequate, atmospheric LES provides a trustworthy representation of the high order moments of the concentration field, up to the fourth order, for a dispersing plume.

Identifiants

pubmed: 32801384
doi: 10.1007/s10546-020-00537-6
pii: 537
pmc: PMC7392951
doi:

Types de publication

Journal Article

Langues

eng

Pagination

291-327

Informations de copyright

© The Author(s) 2020.

Références

Proc Natl Acad Sci U S A. 2002 Oct 1;99(20):12589-93
pubmed: 12228727
Phys Rev E Stat Nonlin Soft Matter Phys. 2011 Sep;84(3 Pt 2):036306
pubmed: 22060491
Environ Pollut. 2016 Jan;208(Pt A):271-283
pubmed: 26282585

Auteurs

Hamidreza Ardeshiri (H)

NILU-Norwegian Institute for Air Research, 2007 Kjeller, Norway.

Massimo Cassiani (M)

NILU-Norwegian Institute for Air Research, 2007 Kjeller, Norway.

Soon Young Park (SY)

Gwangju Institute of Science and Technology, Gwangju, 61005 South Korea.

Andreas Stohl (A)

Department of Meteorology and Geophysics, University of Vienna, 1010 Vienna, Austria.

Ignacio Pisso (I)

NILU-Norwegian Institute for Air Research, 2007 Kjeller, Norway.

Anna Solvejg Dinger (AS)

NILU-Norwegian Institute for Air Research, 2007 Kjeller, Norway.

Classifications MeSH