Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon
Autor(a) principal: | |
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Data de Publicação: | 2015 |
Outros Autores: | , , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Repositório Institucional do INPA |
Texto Completo: | https://repositorio.inpa.gov.br/handle/1/15885 |
Resumo: | The aim of this study was to evaluate how the occurrence of nocturnal Low Level Jets (LLJs) may influence the atmospheric turbulence structure and atmospheric stability at the surface. Using data collected from both radiosondes and Eddy Covariance Systems during the WetAMC-LBA campaign, three atmospheric stability regimes were defined at the surface: weakly stable; transition, and very stable. Relating these regimes and the turbulence structure of strong, weak-type 1 (occurring above 500 m) and weak-type 2 (occurring below 500 m) LLJs, it was observed that 22% of the strong LLJ cases were within the weakly stable regime, whereas only 3% of the weak LLJ cases (type 1 and 2) were in this regime. Another interesting result is that in the weak type 1 LLJ cases, the highest percentage were within the very stable regime (approximately 54%). During strong-LLJs, mean friction velocity and mean turbulence kinetic energy were 0.09 ms-1 and 0.13 m2s-2, respectively. For weak-type 1-LLJs, these variables presented respectively values of 0.04 ms-1 and 0.02 m2 s-2, whereas for weak-type 2-LLJs values were 0.06 ms-1 and 0.03 m2s-2, respectively. These results suggest that LLJs with sufficiently high velocities may increase turbulence and introduce weak atmospheric stability at near surface, depending on the height of occurrence. © 2015, Sociedade Brasileira de Meteorologia. All rights reserved. |
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Santana, Raoni Aquino Silva daTóta, Júliodos Santos, Rosa Maria NascimentoVale, Roseilson Santos do2020-05-19T21:03:15Z2020-05-19T21:03:15Z2015https://repositorio.inpa.gov.br/handle/1/1588510.1590/0102-778620140132The aim of this study was to evaluate how the occurrence of nocturnal Low Level Jets (LLJs) may influence the atmospheric turbulence structure and atmospheric stability at the surface. Using data collected from both radiosondes and Eddy Covariance Systems during the WetAMC-LBA campaign, three atmospheric stability regimes were defined at the surface: weakly stable; transition, and very stable. Relating these regimes and the turbulence structure of strong, weak-type 1 (occurring above 500 m) and weak-type 2 (occurring below 500 m) LLJs, it was observed that 22% of the strong LLJ cases were within the weakly stable regime, whereas only 3% of the weak LLJ cases (type 1 and 2) were in this regime. Another interesting result is that in the weak type 1 LLJ cases, the highest percentage were within the very stable regime (approximately 54%). During strong-LLJs, mean friction velocity and mean turbulence kinetic energy were 0.09 ms-1 and 0.13 m2s-2, respectively. For weak-type 1-LLJs, these variables presented respectively values of 0.04 ms-1 and 0.02 m2 s-2, whereas for weak-type 2-LLJs values were 0.06 ms-1 and 0.03 m2s-2, respectively. These results suggest that LLJs with sufficiently high velocities may increase turbulence and introduce weak atmospheric stability at near surface, depending on the height of occurrence. © 2015, Sociedade Brasileira de Meteorologia. All rights reserved.Volume 30, Número 4, Pags. 405-414Attribution-NonCommercial-NoDerivs 3.0 Brazilhttp://creativecommons.org/licenses/by-nc-nd/3.0/br/info:eu-repo/semantics/openAccessStability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazonEstabilidade e estrutura da turbulência sob a influência de jatos de baixos níveis noturnos no sudoeste da amazôniainfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleRevista Brasileira de Meteorologiaporreponame:Repositório Institucional do INPAinstname:Instituto Nacional de Pesquisas da Amazônia (INPA)instacron:INPAORIGINALartigo-inpa.pdfartigo-inpa.pdfapplication/pdf944149https://repositorio.inpa.gov.br/bitstream/1/15885/1/artigo-inpa.pdfd7633da9835d37e42916a946c5677c0cMD511/158852020-05-19 17:59:07.935oai:repositorio:1/15885Repositório de PublicaçõesPUBhttps://repositorio.inpa.gov.br/oai/requestopendoar:2020-05-19T21:59:07Repositório Institucional do INPA - Instituto Nacional de Pesquisas da Amazônia (INPA)false |
dc.title.en.fl_str_mv |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
dc.title.alternative.pt_BR.fl_str_mv |
Estabilidade e estrutura da turbulência sob a influência de jatos de baixos níveis noturnos no sudoeste da amazônia |
title |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
spellingShingle |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon Santana, Raoni Aquino Silva da |
title_short |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
title_full |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
title_fullStr |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
title_full_unstemmed |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
title_sort |
Stability and turbulence structure under the influence of the nocturnal low level jets in the southwestern amazon |
author |
Santana, Raoni Aquino Silva da |
author_facet |
Santana, Raoni Aquino Silva da Tóta, Júlio dos Santos, Rosa Maria Nascimento Vale, Roseilson Santos do |
author_role |
author |
author2 |
Tóta, Júlio dos Santos, Rosa Maria Nascimento Vale, Roseilson Santos do |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Santana, Raoni Aquino Silva da Tóta, Júlio dos Santos, Rosa Maria Nascimento Vale, Roseilson Santos do |
description |
The aim of this study was to evaluate how the occurrence of nocturnal Low Level Jets (LLJs) may influence the atmospheric turbulence structure and atmospheric stability at the surface. Using data collected from both radiosondes and Eddy Covariance Systems during the WetAMC-LBA campaign, three atmospheric stability regimes were defined at the surface: weakly stable; transition, and very stable. Relating these regimes and the turbulence structure of strong, weak-type 1 (occurring above 500 m) and weak-type 2 (occurring below 500 m) LLJs, it was observed that 22% of the strong LLJ cases were within the weakly stable regime, whereas only 3% of the weak LLJ cases (type 1 and 2) were in this regime. Another interesting result is that in the weak type 1 LLJ cases, the highest percentage were within the very stable regime (approximately 54%). During strong-LLJs, mean friction velocity and mean turbulence kinetic energy were 0.09 ms-1 and 0.13 m2s-2, respectively. For weak-type 1-LLJs, these variables presented respectively values of 0.04 ms-1 and 0.02 m2 s-2, whereas for weak-type 2-LLJs values were 0.06 ms-1 and 0.03 m2s-2, respectively. These results suggest that LLJs with sufficiently high velocities may increase turbulence and introduce weak atmospheric stability at near surface, depending on the height of occurrence. © 2015, Sociedade Brasileira de Meteorologia. All rights reserved. |
publishDate |
2015 |
dc.date.issued.fl_str_mv |
2015 |
dc.date.accessioned.fl_str_mv |
2020-05-19T21:03:15Z |
dc.date.available.fl_str_mv |
2020-05-19T21:03:15Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://repositorio.inpa.gov.br/handle/1/15885 |
dc.identifier.doi.none.fl_str_mv |
10.1590/0102-778620140132 |
url |
https://repositorio.inpa.gov.br/handle/1/15885 |
identifier_str_mv |
10.1590/0102-778620140132 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.ispartof.pt_BR.fl_str_mv |
Volume 30, Número 4, Pags. 405-414 |
dc.rights.driver.fl_str_mv |
Attribution-NonCommercial-NoDerivs 3.0 Brazil http://creativecommons.org/licenses/by-nc-nd/3.0/br/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Attribution-NonCommercial-NoDerivs 3.0 Brazil http://creativecommons.org/licenses/by-nc-nd/3.0/br/ |
eu_rights_str_mv |
openAccess |
dc.publisher.none.fl_str_mv |
Revista Brasileira de Meteorologia |
publisher.none.fl_str_mv |
Revista Brasileira de Meteorologia |
dc.source.none.fl_str_mv |
reponame:Repositório Institucional do INPA instname:Instituto Nacional de Pesquisas da Amazônia (INPA) instacron:INPA |
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Instituto Nacional de Pesquisas da Amazônia (INPA) |
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INPA |
institution |
INPA |
reponame_str |
Repositório Institucional do INPA |
collection |
Repositório Institucional do INPA |
bitstream.url.fl_str_mv |
https://repositorio.inpa.gov.br/bitstream/1/15885/1/artigo-inpa.pdf |
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d7633da9835d37e42916a946c5677c0c |
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Repositório Institucional do INPA - Instituto Nacional de Pesquisas da Amazônia (INPA) |
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