LOGIN / Acesse o sistema

Esqueceu sua senha? Redefina aqui.

Ainda não possui uma conta? Cadastre-se aqui!

REDEFINIR SENHA

Insira o endereço de email associado à sua conta que enviaremos um link de redefinição de senha para você.

Ainda não possui uma conta? Cadastre-se aqui!

Este conteúdo é exclusivo para membros ABCM

Inscreva-se e faça parte da comunidade

CADASTRE-SE

Tem uma conta?

Torne-se um membros ABCM

Veja algumas vantagens em se manter como nosso Associado:

Acesso regular ao JBSMSE
Boletim de notícias ABCM
Acesso livre aos Anais de Eventos
Possibilidade de concorrer às Bolsas de Iniciação Científica da ABCM.
Descontos nos eventos promovidos pela ABCM e pelas entidades com as quais mmantém acordo de cooperação.
Estudantes de gradução serão isentos no primeiro ano de afiliação.
10% de desconto para o Associado que pagar anuidade anntes de completar os 12 meses da última anuidade paga.
Desconto na compra dos livros da ABCM, entre eles: "Engenharia de Dutos" e "Escoamento Multifásico".
CADASTRE-SE SEGUIR PARA O VIDEO >

Tem uma conta?

Eventos Anais de eventos

Anais de eventos

ENCIT 2020

18th Brazilian Congress of Thermal Sciences and Engineering

DEVELOPMENT AND PARAMETRIC ANALYSIS OF A NUMERICAL WIND FLOW MODEL FOR COMPLEX TERRAIN IN OPENFOAM

Submission Author: Gabriel Dumont , RS
Co-Authors: Gabriel Dumont, Adriane Prisco Petry, William C. Radünz
Presenter: Gabriel Dumont

doi://10.26678/ABCM.ENCIT2020.CIT20-0732

 

Abstract

This work is based on the CFD modelling of atmospheric boundary layer flows over complex terrains. The employed CFD toolbox is OpenFOAM, which stands out as a robust open source alternative to conventional programs, and the studied cases involve computational domains based on two real life hills – Askervein Hill in Scotland and Bolund Hill in Denmark, the latter being a highly complex terrain. The model is validated through a simulation in a two-dimensional plain terrain with uniform rugosity, where the atmospheric surface layer profile should remain unchanged; this is achieved by modifying the standard wall functions and altering the constants of the standard k-ε turbulence model. After validation, the model is applied to computational domains which include the hills, and a sensitivity analysis is undertaken by varying mesh refinement, the employed divergence scheme, and the turbulence model’s parameters. The results showed that all models underpredicted the turbulent kinetic energy at the lee of both hills, though the effect is much more pronounced in simulations that used the upwind scheme, probably due to numerical diffusion; however, although the higher-order schemes better predict the steep turbulent kinetic energy gradients, they may also overpredict the velocity gradients in the regions close to the ground. As for the turbulence models, it was shown that determining the constants by fitting meteorological data did not necessarily lead to a better result. In general, especially for regions above 2 meters, simulations that employed modified constants for the k-ε model and higher-order divergence schemes presented wind profiles that were in better agreement with the measured data, with a relative error under 25% for both hills.

Keywords

atmospheric boundary layer, Complex terrain, Parametric analysis, OpenFOAM

 

DOWNLOAD PDF VIEW PRESENTATION

 

‹ voltar para anais de eventos ABCM