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Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES

Bibliographic Details
Main Author: Maldaner, Silvana
Publication Date: 2010
Format: Master thesis
Language: por
Source: Manancial - Repositório Digital da UFSM
dARK ID: ark:/26339/001300000d5fq
Download full: http://repositorio.ufsm.br/handle/1/10255
Summary: The planetary boundary layer (PBL) is a physical system presenting a variety of complex states characterized by the turbulence phenomenon. An understanding of the turbulence patterns and its structural details is of fundamental importance in large and small meteorological scales and atmospheric dispersion. From the numerical point of view, the PBL turbulence has been investigated employing LES models. In LES, only the energy-containing eddies of the degrees of freedom of the turbulent field are explicitly resolved and the effect of the smaller, more isotropic eddies, needs to be parameterized. Modeling these residual turbulent motions, which are also termed subfilter-scale motions, is in large part a phenomenological procedure based on heuristic arguments. These movements are called subfiltro or subgrade and the description of its effects is a major problem in the formulation models of large eddy simulation. Therefore, the derivation of subfilter viscosities expressed in terms of a cutoff wave number is a fundamental procedure in LES methodology. The purpose of the present study is to derive a new turbulent subfilter viscosity based on the energy at cutoff from the Taylor statistical diffusion theory. As an additional purpose, this new viscosity is used in a LES model to obtain a new profile of the vertical velocity skewness in the convective boundary layer (CBL). A comparison between the results of the skewness generated by the LES simulation with the observed skewness values in surface shows that the calculated numerically values are consistent with those observed. Vertical profiles of the simulated skewness by the LES is employed in a Lagrangian stochastic diffusion model to reproduce the contaminants concentrations measured during the Prairie Grass experiment. This new profile simulated from the LES can be used in diffusion models to reproduce the observed contaminants concentrations.
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spelling Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LESDerivation of the vertical velocity skewness from LES modelDispersão de contaminantesTurbulênciaModelos LESCNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIAThe planetary boundary layer (PBL) is a physical system presenting a variety of complex states characterized by the turbulence phenomenon. An understanding of the turbulence patterns and its structural details is of fundamental importance in large and small meteorological scales and atmospheric dispersion. From the numerical point of view, the PBL turbulence has been investigated employing LES models. In LES, only the energy-containing eddies of the degrees of freedom of the turbulent field are explicitly resolved and the effect of the smaller, more isotropic eddies, needs to be parameterized. Modeling these residual turbulent motions, which are also termed subfilter-scale motions, is in large part a phenomenological procedure based on heuristic arguments. These movements are called subfiltro or subgrade and the description of its effects is a major problem in the formulation models of large eddy simulation. Therefore, the derivation of subfilter viscosities expressed in terms of a cutoff wave number is a fundamental procedure in LES methodology. The purpose of the present study is to derive a new turbulent subfilter viscosity based on the energy at cutoff from the Taylor statistical diffusion theory. As an additional purpose, this new viscosity is used in a LES model to obtain a new profile of the vertical velocity skewness in the convective boundary layer (CBL). A comparison between the results of the skewness generated by the LES simulation with the observed skewness values in surface shows that the calculated numerically values are consistent with those observed. Vertical profiles of the simulated skewness by the LES is employed in a Lagrangian stochastic diffusion model to reproduce the contaminants concentrations measured during the Prairie Grass experiment. This new profile simulated from the LES can be used in diffusion models to reproduce the observed contaminants concentrations.A camada limite planetária (CLP) é um sistema físico que apresenta uma variedade de estados complexos caracterizados pelo fenômeno da turbulência. O entendimento dos padrões de turbulência e os seus detalhes estruturais é de fundamental importância nas grandes e pequenas escalas meteorológicas e na dispersão atmosférica. Do ponto de vista numérico, a turbulência na CLP tem sido investigada empregando Large Eddy Simulation Models (LES). Nos modelos de Simulação dos Grandes Turbilhões, os graus de liberdade contendo a energia principal do campo turbulento são resolvidos explicitamente, enquanto o efeito dos menores e mais isotrópicos é parametrizado. A modelagem destes movimentos turbulentos menores e residuais é normalmente baseada em argumentos heurísticos. Tais movimentos são também chamados de subfiltro ou subgrade e a descrição dos seus efeitos constitui um problema fundamental na construção de modelos de Simulação dos Grandes Turbilhões. Desta forma, a derivação de viscosidades de subfiltro expressa em termos do número de onda de corte é um procedimento fundamental na metodologia LES. O objetivo do presente estudo é derivar uma nova viscosidade turbulenta de subfiltro baseada teoria de difusão estatística de Taylor. Como um objetivo adicional, esta nova viscosidade será empregada em um modelo LES para se obter um novo perfil do skewness da velocidade vertical turbulenta na camada limite convectiva (CBL). Uma comparação entre os resultados do skewness gerado pela simulação LES com dados observados do skewness na superfície mostra que os valores modelados estão de acordo com os observados. O perfil vertical do skewness simulado pelo LES é empregado em um modelo estocástico de difusão Lagrangiano para reproduzir as concentrações de contaminantes medidas durante o experimento de Prairie Grass. Este novo perfil de skewness simulado a partir do LES pode ser usado em modelos de difusão para reproduzir concentrações observadas de contaminantes.Universidade Federal de Santa MariaBRMeteorologiaUFSMPrograma de Pós-Graduação em MeteorologiaDegrazia, Gervásio Anneshttp://lattes.cnpq.br/3195210233978887Carvalho, Jonas da Costahttp://lattes.cnpq.br/4338284890563991Roberti, Débora Reginahttp://lattes.cnpq.br/6952076109453197Maldaner, Silvana2010-10-052010-10-052010-08-13info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisapplication/pdfapplication/pdfMALDANER, Silvana. Derivation of the vertical velocity skewness from LES model. 2010. 81 f. Dissertação (Mestrado em Geociências) - Universidade Federal de Santa Maria, Santa Maria, 2010.http://repositorio.ufsm.br/handle/1/10255ark:/26339/001300000d5fqporinfo:eu-repo/semantics/openAccessreponame:Manancial - Repositório Digital da UFSMinstname:Universidade Federal de Santa Maria (UFSM)instacron:UFSM2022-03-02T19:57:31Zoai:repositorio.ufsm.br:1/10255Biblioteca Digital de Teses e Dissertaçõeshttps://repositorio.ufsm.br/PUBhttps://repositorio.ufsm.br/oai/requestatendimento.sib@ufsm.br||tedebc@gmail.com||manancial@ufsm.bropendoar:2022-03-02T19:57:31Manancial - Repositório Digital da UFSM - Universidade Federal de Santa Maria (UFSM)false
dc.title.none.fl_str_mv Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
Derivation of the vertical velocity skewness from LES model
title Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
spellingShingle Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
Maldaner, Silvana
Dispersão de contaminantes
Turbulência
Modelos LES
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA
title_short Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
title_full Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
title_fullStr Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
title_full_unstemmed Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
title_sort Derivação de um skewness da velocidade vertical turbulenta a partir de um modelo LES
author Maldaner, Silvana
author_facet Maldaner, Silvana
author_role author
dc.contributor.none.fl_str_mv Degrazia, Gervásio Annes
http://lattes.cnpq.br/3195210233978887
Carvalho, Jonas da Costa
http://lattes.cnpq.br/4338284890563991
Roberti, Débora Regina
http://lattes.cnpq.br/6952076109453197
dc.contributor.author.fl_str_mv Maldaner, Silvana
dc.subject.por.fl_str_mv Dispersão de contaminantes
Turbulência
Modelos LES
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA
topic Dispersão de contaminantes
Turbulência
Modelos LES
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA
description The planetary boundary layer (PBL) is a physical system presenting a variety of complex states characterized by the turbulence phenomenon. An understanding of the turbulence patterns and its structural details is of fundamental importance in large and small meteorological scales and atmospheric dispersion. From the numerical point of view, the PBL turbulence has been investigated employing LES models. In LES, only the energy-containing eddies of the degrees of freedom of the turbulent field are explicitly resolved and the effect of the smaller, more isotropic eddies, needs to be parameterized. Modeling these residual turbulent motions, which are also termed subfilter-scale motions, is in large part a phenomenological procedure based on heuristic arguments. These movements are called subfiltro or subgrade and the description of its effects is a major problem in the formulation models of large eddy simulation. Therefore, the derivation of subfilter viscosities expressed in terms of a cutoff wave number is a fundamental procedure in LES methodology. The purpose of the present study is to derive a new turbulent subfilter viscosity based on the energy at cutoff from the Taylor statistical diffusion theory. As an additional purpose, this new viscosity is used in a LES model to obtain a new profile of the vertical velocity skewness in the convective boundary layer (CBL). A comparison between the results of the skewness generated by the LES simulation with the observed skewness values in surface shows that the calculated numerically values are consistent with those observed. Vertical profiles of the simulated skewness by the LES is employed in a Lagrangian stochastic diffusion model to reproduce the contaminants concentrations measured during the Prairie Grass experiment. This new profile simulated from the LES can be used in diffusion models to reproduce the observed contaminants concentrations.
publishDate 2010
dc.date.none.fl_str_mv 2010-10-05
2010-10-05
2010-08-13
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.uri.fl_str_mv MALDANER, Silvana. Derivation of the vertical velocity skewness from LES model. 2010. 81 f. Dissertação (Mestrado em Geociências) - Universidade Federal de Santa Maria, Santa Maria, 2010.
http://repositorio.ufsm.br/handle/1/10255
dc.identifier.dark.fl_str_mv ark:/26339/001300000d5fq
identifier_str_mv MALDANER, Silvana. Derivation of the vertical velocity skewness from LES model. 2010. 81 f. Dissertação (Mestrado em Geociências) - Universidade Federal de Santa Maria, Santa Maria, 2010.
ark:/26339/001300000d5fq
url http://repositorio.ufsm.br/handle/1/10255
dc.language.iso.fl_str_mv por
language por
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Universidade Federal de Santa Maria
BR
Meteorologia
UFSM
Programa de Pós-Graduação em Meteorologia
publisher.none.fl_str_mv Universidade Federal de Santa Maria
BR
Meteorologia
UFSM
Programa de Pós-Graduação em Meteorologia
dc.source.none.fl_str_mv reponame:Manancial - Repositório Digital da UFSM
instname:Universidade Federal de Santa Maria (UFSM)
instacron:UFSM
instname_str Universidade Federal de Santa Maria (UFSM)
instacron_str UFSM
institution UFSM
reponame_str Manancial - Repositório Digital da UFSM
collection Manancial - Repositório Digital da UFSM
repository.name.fl_str_mv Manancial - Repositório Digital da UFSM - Universidade Federal de Santa Maria (UFSM)
repository.mail.fl_str_mv atendimento.sib@ufsm.br||tedebc@gmail.com||manancial@ufsm.br
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