High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF

Detalhes bibliográficos
Autor(a) principal: Comin, Alcimoni Nelci
Data de Publicação: 2016
Outros Autores: Acevedo, Otávio Costa, Souza, Ronald Buss de
Tipo de documento: Artigo
Idioma: por
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/7020
Resumo: This paper presents run high-resolution Weather Research and Forecasting (WRF) model in the region of South Shetland Islands, in Antarctica. Simulation model are compared to observations taken aboard a Polar Ship during the transect in this region. A total of 4 different simulations were performed, varying the number of points of the innermost domain 127 x 127 and 187 x 187  and two microphysics schemes. The results of air temperature and dew point are highly dependent on the size of the internal domain. When the small domain with points 127 are used, the model produces abrupt fluctuations of these variables and highly underestimates them in both settings. This can be attributed the sensitivity of the model to the transfer of information between the different nested grids. With larger innermost grid with points 187, such fluctuations no longer occur. The underestimation temperatures in the WRF model is associated with the deficiency representation on days with stratiform cloudiness. Days with middle-level clouds model the temperature tend to be better represented.  The air pressure is adequately simulated with both domains, as it is more dependent on large-scale weather patterns, derived from the global model, which provides the boundary conditions. The small differences in air pressure among the simulations are a consequence of the dynamical adjustment of the model. The microphysics scheme WSM5 results were better than scheme WSM3 for all variables tested here.
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spelling High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRFSimulação Numérica em Alta Resolução nas Ilhas Shetland do Sul, Antártica, Usando WRFWRF; High-resolution; South Shetland Islands; Polar Ship.WRF; Alta resolução; Ilhas Shetland do Sul; Navio Polar.This paper presents run high-resolution Weather Research and Forecasting (WRF) model in the region of South Shetland Islands, in Antarctica. Simulation model are compared to observations taken aboard a Polar Ship during the transect in this region. A total of 4 different simulations were performed, varying the number of points of the innermost domain 127 x 127 and 187 x 187  and two microphysics schemes. The results of air temperature and dew point are highly dependent on the size of the internal domain. When the small domain with points 127 are used, the model produces abrupt fluctuations of these variables and highly underestimates them in both settings. This can be attributed the sensitivity of the model to the transfer of information between the different nested grids. With larger innermost grid with points 187, such fluctuations no longer occur. The underestimation temperatures in the WRF model is associated with the deficiency representation on days with stratiform cloudiness. Days with middle-level clouds model the temperature tend to be better represented.  The air pressure is adequately simulated with both domains, as it is more dependent on large-scale weather patterns, derived from the global model, which provides the boundary conditions. The small differences in air pressure among the simulations are a consequence of the dynamical adjustment of the model. The microphysics scheme WSM5 results were better than scheme WSM3 for all variables tested here.Este artigo apresenta simulações de alta resolução com o modelo Weather Research and Forecasting (WRF) para a Ilhas Shetland do Sul, na Antártica. Os dados observados são coletadas pelos sensores instalados no navio Polar durante o transecto nesta região. Este estudo incluiu quatro simulações diferentes; variando o número de pontos de grade no domínio interno entre 127 x 127 e 187 x 187 e duas configurações de microfísica.  As simulações para a temperatura do ar e ponto de orvalho são altamente dependente do número de pontos de grade do domínio interno. Quando o domínio com 127 pontos é usado o modelo reproduz flutuações abruptas dessas variáveis e altas subestimativas em ambas as configurações. Isto pode ser atribuído à sensibilidade associada à transferência de informações entre as diferentes grades aninhadas. Com a expansão da grade interna em 187 pontos as flutuações deixam de ocorrer. A subestimativa das temperaturas no modelo WRF também é associada com a deficiência na representação de nebulosidade estratiforme. Nos dias com nebulosidade média o modelo simula melhor essas variáveis.  Já a pressão é adequadamente simulada com os dois domínios e é mais dependente de padrões climáticos de grande escala derivadas do modelo global. As pequenas diferenças na pressão são devido ao ajuste dinâmico do modelo. O esquema microfísico WSM5 apresenta resultados melhores que o WSM3 para todas as variáveis testadas aqui.Universidade Federal do Rio de Janeiro2016-10-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/702010.11137/2016_3_105_110Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 105-110Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 105-1101982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/7020/5587Copyright (c) 2016 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessComin, Alcimoni NelciAcevedo, Otávio CostaSouza, Ronald Buss de2017-02-15T18:21:53Zoai:www.revistas.ufrj.br:article/7020Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-02-15T18:21:53Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
Simulação Numérica em Alta Resolução nas Ilhas Shetland do Sul, Antártica, Usando WRF
title High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
spellingShingle High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
Comin, Alcimoni Nelci
WRF; High-resolution; South Shetland Islands; Polar Ship.
WRF; Alta resolução; Ilhas Shetland do Sul; Navio Polar.
title_short High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
title_full High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
title_fullStr High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
title_full_unstemmed High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
title_sort High-Resolution Numerical Weather Simulation at the South Shetland Islands, Antarctic, Using WRF
author Comin, Alcimoni Nelci
author_facet Comin, Alcimoni Nelci
Acevedo, Otávio Costa
Souza, Ronald Buss de
author_role author
author2 Acevedo, Otávio Costa
Souza, Ronald Buss de
author2_role author
author
dc.contributor.author.fl_str_mv Comin, Alcimoni Nelci
Acevedo, Otávio Costa
Souza, Ronald Buss de
dc.subject.por.fl_str_mv WRF; High-resolution; South Shetland Islands; Polar Ship.
WRF; Alta resolução; Ilhas Shetland do Sul; Navio Polar.
topic WRF; High-resolution; South Shetland Islands; Polar Ship.
WRF; Alta resolução; Ilhas Shetland do Sul; Navio Polar.
description This paper presents run high-resolution Weather Research and Forecasting (WRF) model in the region of South Shetland Islands, in Antarctica. Simulation model are compared to observations taken aboard a Polar Ship during the transect in this region. A total of 4 different simulations were performed, varying the number of points of the innermost domain 127 x 127 and 187 x 187  and two microphysics schemes. The results of air temperature and dew point are highly dependent on the size of the internal domain. When the small domain with points 127 are used, the model produces abrupt fluctuations of these variables and highly underestimates them in both settings. This can be attributed the sensitivity of the model to the transfer of information between the different nested grids. With larger innermost grid with points 187, such fluctuations no longer occur. The underestimation temperatures in the WRF model is associated with the deficiency representation on days with stratiform cloudiness. Days with middle-level clouds model the temperature tend to be better represented.  The air pressure is adequately simulated with both domains, as it is more dependent on large-scale weather patterns, derived from the global model, which provides the boundary conditions. The small differences in air pressure among the simulations are a consequence of the dynamical adjustment of the model. The microphysics scheme WSM5 results were better than scheme WSM3 for all variables tested here.
publishDate 2016
dc.date.none.fl_str_mv 2016-10-03
dc.type.none.fl_str_mv
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/7020
10.11137/2016_3_105_110
url https://revistas.ufrj.br/index.php/aigeo/article/view/7020
identifier_str_mv 10.11137/2016_3_105_110
dc.language.iso.fl_str_mv por
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dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/7020/5587
dc.rights.driver.fl_str_mv Copyright (c) 2016 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2016 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 105-110
Anuário do Instituto de Geociências; Vol 39, No 3 (2016); 105-110
1982-3908
0101-9759
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reponame_str Anuário do Instituto de Geociências (Online)
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