Techniques for Lagrangian modelling of dispersion in geophysical flows

Basic concepts and definitions relative to Lagrangian Particle Dispersion Models (LPDMs)for the description of turbulent dispersion are introduced. The study focusses on LPDMs that use as input, for the large scale motion, fields produced by Eulerian models, with the small scale motions described b...

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Main Author: Rossi, Daniele <1984>
Other Authors: Tampieri, Francesco
Format: Doctoral Thesis
Language:en
Published: Alma Mater Studiorum - Università di Bologna 2014
Subjects:
Online Access:http://amsdottorato.unibo.it/6356/
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spelling ndltd-unibo.it-oai-amsdottorato.cib.unibo.it-63562014-10-09T04:47:26Z Techniques for Lagrangian modelling of dispersion in geophysical flows Rossi, Daniele <1984> FIS/06 Fisica per il sistema terra e il mezzo circumterrestre Basic concepts and definitions relative to Lagrangian Particle Dispersion Models (LPDMs)for the description of turbulent dispersion are introduced. The study focusses on LPDMs that use as input, for the large scale motion, fields produced by Eulerian models, with the small scale motions described by Lagrangian Stochastic Models (LSMs). The data of two different dynamical model have been used: a Large Eddy Simulation (LES) and a General Circulation Model (GCM). After reviewing the small scale closure adopted by the Eulerian model, the development and implementation of appropriate LSMs is outlined. The basic requirement of every LPDM used in this work is its fullfillment of the Well Mixed Condition (WMC). For the dispersion description in the GCM domain, a stochastic model of Markov order 0, consistent with the eddy-viscosity closure of the dynamical model, is implemented. A LSM of Markov order 1, more suitable for shorter timescales, has been implemented for the description of the unresolved motion of the LES fields. Different assumptions on the small scale correlation time are made. Tests of the LSM on GCM fields suggest that the use of an interpolation algorithm able to maintain an analytical consistency between the diffusion coefficient and its derivative is mandatory if the model has to satisfy the WMC. Also a dynamical time step selection scheme based on the diffusion coefficient shape is introduced, and the criteria for the integration step selection are discussed. Absolute and relative dispersion experiments are made with various unresolved motion settings for the LSM on LES data, and the results are compared with laboratory data. The study shows that the unresolved turbulence parameterization has a negligible influence on the absolute dispersion, while it affects the contribution of the relative dispersion and meandering to absolute dispersion, as well as the Lagrangian correlation. Alma Mater Studiorum - Università di Bologna Tampieri, Francesco 2014-04-07 Doctoral Thesis PeerReviewed application/pdf en http://amsdottorato.unibo.it/6356/ info:eu-repo/semantics/openAccess
collection NDLTD
language en
format Doctoral Thesis
sources NDLTD
topic FIS/06 Fisica per il sistema terra e il mezzo circumterrestre
spellingShingle FIS/06 Fisica per il sistema terra e il mezzo circumterrestre
Rossi, Daniele <1984>
Techniques for Lagrangian modelling of dispersion in geophysical flows
description Basic concepts and definitions relative to Lagrangian Particle Dispersion Models (LPDMs)for the description of turbulent dispersion are introduced. The study focusses on LPDMs that use as input, for the large scale motion, fields produced by Eulerian models, with the small scale motions described by Lagrangian Stochastic Models (LSMs). The data of two different dynamical model have been used: a Large Eddy Simulation (LES) and a General Circulation Model (GCM). After reviewing the small scale closure adopted by the Eulerian model, the development and implementation of appropriate LSMs is outlined. The basic requirement of every LPDM used in this work is its fullfillment of the Well Mixed Condition (WMC). For the dispersion description in the GCM domain, a stochastic model of Markov order 0, consistent with the eddy-viscosity closure of the dynamical model, is implemented. A LSM of Markov order 1, more suitable for shorter timescales, has been implemented for the description of the unresolved motion of the LES fields. Different assumptions on the small scale correlation time are made. Tests of the LSM on GCM fields suggest that the use of an interpolation algorithm able to maintain an analytical consistency between the diffusion coefficient and its derivative is mandatory if the model has to satisfy the WMC. Also a dynamical time step selection scheme based on the diffusion coefficient shape is introduced, and the criteria for the integration step selection are discussed. Absolute and relative dispersion experiments are made with various unresolved motion settings for the LSM on LES data, and the results are compared with laboratory data. The study shows that the unresolved turbulence parameterization has a negligible influence on the absolute dispersion, while it affects the contribution of the relative dispersion and meandering to absolute dispersion, as well as the Lagrangian correlation.
author2 Tampieri, Francesco
author_facet Tampieri, Francesco
Rossi, Daniele <1984>
author Rossi, Daniele <1984>
author_sort Rossi, Daniele <1984>
title Techniques for Lagrangian modelling of dispersion in geophysical flows
title_short Techniques for Lagrangian modelling of dispersion in geophysical flows
title_full Techniques for Lagrangian modelling of dispersion in geophysical flows
title_fullStr Techniques for Lagrangian modelling of dispersion in geophysical flows
title_full_unstemmed Techniques for Lagrangian modelling of dispersion in geophysical flows
title_sort techniques for lagrangian modelling of dispersion in geophysical flows
publisher Alma Mater Studiorum - Università di Bologna
publishDate 2014
url http://amsdottorato.unibo.it/6356/
work_keys_str_mv AT rossidaniele1984 techniquesforlagrangianmodellingofdispersioningeophysicalflows
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