TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION
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Publication Date: | 2016 |
Other Authors: | , , |
Format: | Article |
Language: | por |
Source: | Revista Ciência e Natura (Online) |
Download full: | https://periodicos.ufsm.br/cienciaenatura/article/view/20243 |
Summary: | The planetary boundary layer (PBL) structure is investigated focusing on days with low-tropospheric ducts occurrence in the Petrolina-PE region, in the period from 1 to 29 April 2014. Ducts identification and the estimative of the PBL top/height and its dynamic and thermodynamic characterization is based on 12 UTC upper-air soundings launched at the altitude station of Petrolina. Surface ducts are associated with high instability and wind speed intensification in the surface layer. Ducts at the PBL top (elevated ducts) are associated with a decrease in the moisture content of the air and a wind speed maximum, above the PBL, in the low-troposphere. |
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TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGIONDutos Troposféricos e a Estrutura da Camada Limite Planetária na Região de PetrolinaRefractivity. PBL. Surface ducts. Elevated ducts. Petrolina.Refratividade. CLP. Dutos de superfície. Dutos elevados. Petrolina.The planetary boundary layer (PBL) structure is investigated focusing on days with low-tropospheric ducts occurrence in the Petrolina-PE region, in the period from 1 to 29 April 2014. Ducts identification and the estimative of the PBL top/height and its dynamic and thermodynamic characterization is based on 12 UTC upper-air soundings launched at the altitude station of Petrolina. Surface ducts are associated with high instability and wind speed intensification in the surface layer. Ducts at the PBL top (elevated ducts) are associated with a decrease in the moisture content of the air and a wind speed maximum, above the PBL, in the low-troposphere.A estrutura da camada limite planetária (CLP) é investigada com foco nos dias com ocorrência de dutos na baixa troposfera na região de Petrolina-PE, no período de 1 a 29 de abril de 2014. A identificação dos dutos e a estimativa do topo/altura da CLP e sua caracterização dinâmica e termodinâmica está fundamentada em dados de sondagens de ar superior realizadas às 12 UTC na estação de altitude de Petrolina. Os dutos de superfície estão associados com alta instabilidade e aumento da intensidade do vento na camada superficial. Os dutos no topo da CLP (dutos elevados) estão associados com uma redução do teor de umidade do ar e um máximo da intensidade do vento, acima da camada, na baixa troposfera.Universidade Federal de Santa Maria2016-07-20info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://periodicos.ufsm.br/cienciaenatura/article/view/2024310.5902/2179460X20243Ciência e Natura; Vol. 38 (2016): SPECIAL EDITION: IX WORKSHOP BRASILEIRO DE MICROMETEOROLOGIA; 318-325Ciência e Natura; v. 38 (2016): EDIÇÃO ESPECIAL: IX WORKSHOP BRASILEIRO DE MICROMETEOROLOGIA; 318-3252179-460X0100-8307reponame:Revista Ciência e Natura (Online)instname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMporhttps://periodicos.ufsm.br/cienciaenatura/article/view/20243/pdfCopyright (c) 2016 Ciência e Naturainfo:eu-repo/semantics/openAccessSousa, Leandro Fontes deCorreia, Magaly de FatimaAragão, Maria Regina da SilvaRibeiro, Roberta Everllyn Pereira2022-10-14T13:33:33Zoai:ojs.pkp.sfu.ca:article/20243Revistahttps://periodicos.ufsm.br/cienciaenatura/indexPUBhttps://periodicos.ufsm.br/cienciaenatura/oaicienciaenatura@ufsm.br || centraldeperiodicos@ufsm.br2179-460X0100-8307opendoar:2022-10-14T13:33:33Revista Ciência e Natura (Online) - Universidade Federal de Santa Maria (UFSM)false |
dc.title.none.fl_str_mv |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION Dutos Troposféricos e a Estrutura da Camada Limite Planetária na Região de Petrolina |
title |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION |
spellingShingle |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION Sousa, Leandro Fontes de Refractivity. PBL. Surface ducts. Elevated ducts. Petrolina. Refratividade. CLP. Dutos de superfície. Dutos elevados. Petrolina. |
title_short |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION |
title_full |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION |
title_fullStr |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION |
title_full_unstemmed |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION |
title_sort |
TROPOSPHERIC DUCTS AND PLANETARY BOUNDARY LAYER STRUCTURE IN THE PETROLINA REGION |
author |
Sousa, Leandro Fontes de |
author_facet |
Sousa, Leandro Fontes de Correia, Magaly de Fatima Aragão, Maria Regina da Silva Ribeiro, Roberta Everllyn Pereira |
author_role |
author |
author2 |
Correia, Magaly de Fatima Aragão, Maria Regina da Silva Ribeiro, Roberta Everllyn Pereira |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Sousa, Leandro Fontes de Correia, Magaly de Fatima Aragão, Maria Regina da Silva Ribeiro, Roberta Everllyn Pereira |
dc.subject.por.fl_str_mv |
Refractivity. PBL. Surface ducts. Elevated ducts. Petrolina. Refratividade. CLP. Dutos de superfície. Dutos elevados. Petrolina. |
topic |
Refractivity. PBL. Surface ducts. Elevated ducts. Petrolina. Refratividade. CLP. Dutos de superfície. Dutos elevados. Petrolina. |
description |
The planetary boundary layer (PBL) structure is investigated focusing on days with low-tropospheric ducts occurrence in the Petrolina-PE region, in the period from 1 to 29 April 2014. Ducts identification and the estimative of the PBL top/height and its dynamic and thermodynamic characterization is based on 12 UTC upper-air soundings launched at the altitude station of Petrolina. Surface ducts are associated with high instability and wind speed intensification in the surface layer. Ducts at the PBL top (elevated ducts) are associated with a decrease in the moisture content of the air and a wind speed maximum, above the PBL, in the low-troposphere. |
publishDate |
2016 |
dc.date.none.fl_str_mv |
2016-07-20 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://periodicos.ufsm.br/cienciaenatura/article/view/20243 10.5902/2179460X20243 |
url |
https://periodicos.ufsm.br/cienciaenatura/article/view/20243 |
identifier_str_mv |
10.5902/2179460X20243 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://periodicos.ufsm.br/cienciaenatura/article/view/20243/pdf |
dc.rights.driver.fl_str_mv |
Copyright (c) 2016 Ciência e Natura info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2016 Ciência e Natura |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
dc.source.none.fl_str_mv |
Ciência e Natura; Vol. 38 (2016): SPECIAL EDITION: IX WORKSHOP BRASILEIRO DE MICROMETEOROLOGIA; 318-325 Ciência e Natura; v. 38 (2016): EDIÇÃO ESPECIAL: IX WORKSHOP BRASILEIRO DE MICROMETEOROLOGIA; 318-325 2179-460X 0100-8307 reponame:Revista Ciência e Natura (Online) instname:Universidade Federal de Santa Maria (UFSM) instacron:UFSM |
instname_str |
Universidade Federal de Santa Maria (UFSM) |
instacron_str |
UFSM |
institution |
UFSM |
reponame_str |
Revista Ciência e Natura (Online) |
collection |
Revista Ciência e Natura (Online) |
repository.name.fl_str_mv |
Revista Ciência e Natura (Online) - Universidade Federal de Santa Maria (UFSM) |
repository.mail.fl_str_mv |
cienciaenatura@ufsm.br || centraldeperiodicos@ufsm.br |
_version_ |
1839277880375246848 |