Simulating Weather Events with a Linked Atmosphere-Hydrology Model

Detalhes bibliográficos
Autor(a) principal: Pereira,Fábio Farias
Data de Publicação: 2020
Outros Autores: Uvo,Cintia Bertacchi
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Revista Brasileira de Meteorologia (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862020000400703
Resumo: Abstract This study aims at assess the importance of a conceptual representation of hydrological processes when modelling atmospheric circulation. It compares results from a regional atmospheric model that interprets land surface hydrological processes based on parameterizations with results from a two-way coupled atmosphere-hydrological model that has a process-based approach to the land surface hydrological cycle. These numerical models were applied to a region covering the Rio Grande basin, Brazil. The same input data, initial and boundary conditions were used on a 31-day simulation period. Results obtained from these simulations were compared to visible satellite images and gauging rainfall stations for three case studies that included a cold front, deep convective clouds and stable atmospheric conditions. Both models could reproduce regional patterns of air circulation and rainfall influenced by the orography of the basin. However, atmospheric processes driven by spatial gradients of land surface temperature or local surface heating were spatially better represented by the atmospheric-hydrological modelling system rather than the regional atmospheric model. Since areas characterized by spatial gradients of land surface temperature and local surface heating were closely associated with convergent air flows near land surface and strong vertical motion in the mid troposphere, this finding enhanced the role of a good representation of land surface hydrological processes for a better modelling the atmospheric dynamics.
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spelling Simulating Weather Events with a Linked Atmosphere-Hydrology ModelEarth surface dynamicsweather eventsatmosphere-hydrology modelsland surface modelingAbstract This study aims at assess the importance of a conceptual representation of hydrological processes when modelling atmospheric circulation. It compares results from a regional atmospheric model that interprets land surface hydrological processes based on parameterizations with results from a two-way coupled atmosphere-hydrological model that has a process-based approach to the land surface hydrological cycle. These numerical models were applied to a region covering the Rio Grande basin, Brazil. The same input data, initial and boundary conditions were used on a 31-day simulation period. Results obtained from these simulations were compared to visible satellite images and gauging rainfall stations for three case studies that included a cold front, deep convective clouds and stable atmospheric conditions. Both models could reproduce regional patterns of air circulation and rainfall influenced by the orography of the basin. However, atmospheric processes driven by spatial gradients of land surface temperature or local surface heating were spatially better represented by the atmospheric-hydrological modelling system rather than the regional atmospheric model. Since areas characterized by spatial gradients of land surface temperature and local surface heating were closely associated with convergent air flows near land surface and strong vertical motion in the mid troposphere, this finding enhanced the role of a good representation of land surface hydrological processes for a better modelling the atmospheric dynamics.Sociedade Brasileira de Meteorologia2020-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862020000400703Revista Brasileira de Meteorologia v.35 n.4 2020reponame:Revista Brasileira de Meteorologia (Online)instname:Sociedade Brasileira de Meteorologia (SBMET)instacron:SBMET10.1590/0102-77863540077info:eu-repo/semantics/openAccessPereira,Fábio FariasUvo,Cintia Bertacchieng2020-12-08T00:00:00Zoai:scielo:S0102-77862020000400703Revistahttp://www.rbmet.org.br/port/index.phpONGhttps://old.scielo.br/oai/scielo-oai.php||rbmet@rbmet.org.br1982-43510102-7786opendoar:2020-12-08T00:00Revista Brasileira de Meteorologia (Online) - Sociedade Brasileira de Meteorologia (SBMET)false
dc.title.none.fl_str_mv Simulating Weather Events with a Linked Atmosphere-Hydrology Model
title Simulating Weather Events with a Linked Atmosphere-Hydrology Model
spellingShingle Simulating Weather Events with a Linked Atmosphere-Hydrology Model
Pereira,Fábio Farias
Earth surface dynamics
weather events
atmosphere-hydrology models
land surface modeling
title_short Simulating Weather Events with a Linked Atmosphere-Hydrology Model
title_full Simulating Weather Events with a Linked Atmosphere-Hydrology Model
title_fullStr Simulating Weather Events with a Linked Atmosphere-Hydrology Model
title_full_unstemmed Simulating Weather Events with a Linked Atmosphere-Hydrology Model
title_sort Simulating Weather Events with a Linked Atmosphere-Hydrology Model
author Pereira,Fábio Farias
author_facet Pereira,Fábio Farias
Uvo,Cintia Bertacchi
author_role author
author2 Uvo,Cintia Bertacchi
author2_role author
dc.contributor.author.fl_str_mv Pereira,Fábio Farias
Uvo,Cintia Bertacchi
dc.subject.por.fl_str_mv Earth surface dynamics
weather events
atmosphere-hydrology models
land surface modeling
topic Earth surface dynamics
weather events
atmosphere-hydrology models
land surface modeling
description Abstract This study aims at assess the importance of a conceptual representation of hydrological processes when modelling atmospheric circulation. It compares results from a regional atmospheric model that interprets land surface hydrological processes based on parameterizations with results from a two-way coupled atmosphere-hydrological model that has a process-based approach to the land surface hydrological cycle. These numerical models were applied to a region covering the Rio Grande basin, Brazil. The same input data, initial and boundary conditions were used on a 31-day simulation period. Results obtained from these simulations were compared to visible satellite images and gauging rainfall stations for three case studies that included a cold front, deep convective clouds and stable atmospheric conditions. Both models could reproduce regional patterns of air circulation and rainfall influenced by the orography of the basin. However, atmospheric processes driven by spatial gradients of land surface temperature or local surface heating were spatially better represented by the atmospheric-hydrological modelling system rather than the regional atmospheric model. Since areas characterized by spatial gradients of land surface temperature and local surface heating were closely associated with convergent air flows near land surface and strong vertical motion in the mid troposphere, this finding enhanced the role of a good representation of land surface hydrological processes for a better modelling the atmospheric dynamics.
publishDate 2020
dc.date.none.fl_str_mv 2020-12-01
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dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/0102-77863540077
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dc.publisher.none.fl_str_mv Sociedade Brasileira de Meteorologia
publisher.none.fl_str_mv Sociedade Brasileira de Meteorologia
dc.source.none.fl_str_mv Revista Brasileira de Meteorologia v.35 n.4 2020
reponame:Revista Brasileira de Meteorologia (Online)
instname:Sociedade Brasileira de Meteorologia (SBMET)
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reponame_str Revista Brasileira de Meteorologia (Online)
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