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dc.contributor.authorArdeshiri, Hamidreza
dc.contributor.authorCassiani, Massimo
dc.contributor.authorPark, Soon-Young
dc.contributor.authorStohl, Andreas
dc.contributor.authorPisso, Ignacio
dc.contributor.authorDinger, Anna Solvejg
dc.date.accessioned2020-08-04T09:45:58Z
dc.date.available2020-08-04T09:45:58Z
dc.date.created2020-07-02T10:08:27Z
dc.date.issued2020
dc.identifier.citationBoundary-layer Meteorology. 2020, 176, 291-327.en_US
dc.identifier.issn0006-8314
dc.identifier.urihttps://hdl.handle.net/11250/2670738
dc.description.abstractLarge-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.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleOn the Convergence and Capability of the Large-Eddy Simulation of Concentration Fluctuations in Passive Plumes for a Neutral Boundary Layer at Infinite Reynolds Numberen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© The Author(s) 2020en_US
dc.source.pagenumber291-327en_US
dc.source.volume176en_US
dc.source.journalBoundary-layer Meteorologyen_US
dc.identifier.doi10.1007/s10546-020-00537-6
dc.identifier.cristin1818217
dc.relation.projectEC/H2020/670462en_US
dc.relation.projectNorges forskningsråd: 294948en_US
dc.relation.projectNotur/NorStore: NN9419Ken_US
dc.relation.projectNotur/NorStore: NS9419Ken_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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