Altura da Camada de Mistura na Cidade do Rio de Janeiro

Detalhes bibliográficos
Autor(a) principal: Ribeiro, Benedito Crescencio
Data de Publicação: 1978
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/5810
Resumo: This work describes the methods for determination of the mixing depths at morning and afternoon hours. In over Rio de Janeiro the morning mixing depth is calculated extending a dry adiabat on the "SKEWT - LOGP" diagram from 12 GMT surface temperature to its intersection with vertical temperature profile, observed at the minimum temperature hours. In the afternoon hours a dry adiabat is extended from maximum surface temperature to Its intersection with the 12 GMT observed vertical temperature profile. The mean mixing depth is calculated for each month over the period 1967-1976 through two distinct ways. The results are very well correlated and show a correlation coefficient greater than 0.9. Over Rio de Janeiro the mean maximum mixing depths are heigher in July (1216 m)and lower in october (812 m). The mean mixing depths in the morning hours are heigher in December (633 m) and lower in June (369 m).
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spelling Altura da Camada de Mistura na Cidade do Rio de JaneiroThis work describes the methods for determination of the mixing depths at morning and afternoon hours. In over Rio de Janeiro the morning mixing depth is calculated extending a dry adiabat on the "SKEWT - LOGP" diagram from 12 GMT surface temperature to its intersection with vertical temperature profile, observed at the minimum temperature hours. In the afternoon hours a dry adiabat is extended from maximum surface temperature to Its intersection with the 12 GMT observed vertical temperature profile. The mean mixing depth is calculated for each month over the period 1967-1976 through two distinct ways. The results are very well correlated and show a correlation coefficient greater than 0.9. Over Rio de Janeiro the mean maximum mixing depths are heigher in July (1216 m)and lower in october (812 m). The mean mixing depths in the morning hours are heigher in December (633 m) and lower in June (369 m).This work describes the methods for determination of the mixing depths at morning and afternoon hours. In over Rio de Janeiro the morning mixing depth is calculated extending a dry adiabat on the "SKEWT - LOGP" diagram from 12 GMT surface temperature to its intersection with vertical temperature profile, observed at the minimum temperature hours. In the afternoon hours a dry adiabat is extended from maximum surface temperature to Its intersection with the 12 GMT observed vertical temperature profile. The mean mixing depth is calculated for each month over the period 1967-1976 through two distinct ways. The results are very well correlated and show a correlation coefficient greater than 0.9. Over Rio de Janeiro the mean maximum mixing depths are heigher in July (1216 m)and lower in october (812 m). The mean mixing depths in the morning hours are heigher in December (633 m) and lower in June (369 m).Universidade Federal do Rio de JaneiroRibeiro, Benedito Crescencio1978-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/581010.11137/1978_0_71-85Anuário do Instituto de Geociências; Vol 2 (1978); 71-85Anuário do Instituto de Geociências; Vol 2 (1978); 71-851982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/5810/4407Copyright (c) 1978 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccess2021-08-04T01:14:45Zoai:www.revistas.ufrj.br:article/5810Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2021-08-04T01:14:45Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv Altura da Camada de Mistura na Cidade do Rio de Janeiro
title Altura da Camada de Mistura na Cidade do Rio de Janeiro
spellingShingle Altura da Camada de Mistura na Cidade do Rio de Janeiro
Ribeiro, Benedito Crescencio
title_short Altura da Camada de Mistura na Cidade do Rio de Janeiro
title_full Altura da Camada de Mistura na Cidade do Rio de Janeiro
title_fullStr Altura da Camada de Mistura na Cidade do Rio de Janeiro
title_full_unstemmed Altura da Camada de Mistura na Cidade do Rio de Janeiro
title_sort Altura da Camada de Mistura na Cidade do Rio de Janeiro
author Ribeiro, Benedito Crescencio
author_facet Ribeiro, Benedito Crescencio
author_role author
dc.contributor.none.fl_str_mv
dc.contributor.author.fl_str_mv Ribeiro, Benedito Crescencio
dc.subject.none.fl_str_mv
description This work describes the methods for determination of the mixing depths at morning and afternoon hours. In over Rio de Janeiro the morning mixing depth is calculated extending a dry adiabat on the "SKEWT - LOGP" diagram from 12 GMT surface temperature to its intersection with vertical temperature profile, observed at the minimum temperature hours. In the afternoon hours a dry adiabat is extended from maximum surface temperature to Its intersection with the 12 GMT observed vertical temperature profile. The mean mixing depth is calculated for each month over the period 1967-1976 through two distinct ways. The results are very well correlated and show a correlation coefficient greater than 0.9. Over Rio de Janeiro the mean maximum mixing depths are heigher in July (1216 m)and lower in october (812 m). The mean mixing depths in the morning hours are heigher in December (633 m) and lower in June (369 m).
publishDate 1978
dc.date.none.fl_str_mv 1978-01-01
dc.type.none.fl_str_mv
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://revistas.ufrj.br/index.php/aigeo/article/view/5810
10.11137/1978_0_71-85
url https://revistas.ufrj.br/index.php/aigeo/article/view/5810
identifier_str_mv 10.11137/1978_0_71-85
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/5810/4407
dc.rights.driver.fl_str_mv Copyright (c) 1978 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 1978 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 2 (1978); 71-85
Anuário do Instituto de Geociências; Vol 2 (1978); 71-85
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
instname:Universidade Federal do Rio de Janeiro (UFRJ)
instacron:UFRJ
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institution UFRJ
reponame_str Anuário do Instituto de Geociências (Online)
collection Anuário do Instituto de Geociências (Online)
repository.name.fl_str_mv Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)
repository.mail.fl_str_mv anuario@igeo.ufrj.br||
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