ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL

Detalhes bibliográficos
Autor(a) principal: Ely, Deise Fabiana
Data de Publicação: 2019
Outros Autores: Kogima, Karitha Campos
Tipo de documento: Artigo
Idioma: por
Título da fonte: Geo UERJ
Texto Completo: https://www.e-publicacoes.uerj.br/geouerj/article/view/40947
Resumo: The purpose of this work is to analyze the variability of the maximum annual temperatures in the state of Paraná from 1976 to 2015 to identify the occurrence of periods of extreme heat. Two different indexes were applied: 1) spring - summer (P - V) and 2) daily index (ID). The P-V index allows you to detect only the most extreme events. It was found that they occur more frequently in the months of November to February. The ID index identifies the anomalous warming events that occur throughout the year. It was found that the largest records occur in the autumn and winter seasons. Analyzing both indices it was possible to discover that the stations located in the northern and western regions of Paraná, mainly those located north of the Tropic of Capricorn, presented more significant heat waves, with longer duration and with higher temperatures. On the other hand, the stations located in the center-south registered heat waves with less intensity and duration. Due to the fact that the heat waves are characterized in different ways by the applied methods, the results are dependent on the index used, so the selection of the criterion to determine the heat waves depends on the purpose of the study.The purpose of this work is to analyze the variability of the maximum annual temperatures in the state of Paraná from 1976 to 2015 to identify the occurrence of periods of extreme heat. Two different indexes were applied: 1) spring - summer (P - V) and 2) daily index (ID). The P-V index allows you to detect only the most extreme events. It was found that they occur more frequently in the months of November to February. The ID index identifies the anomalous warming events that occur throughout the year. It was found that the largest records occur in the autumn and winter seasons. Analyzing both indices it was possible to discover that the stations located in the northern and western regions of Paraná, mainly those located north of the Tropic of Capricorn, presented more significant heat waves, with longer duration and with higher temperatures. On the other hand, the stations located in the center-south registered heat waves with less intensity and duration. Due to the fact that the heat waves are characterized in different ways by the applied methods, the results are dependent on the index used, so the selection of the criterion to determine the heat waves depends on the purpose of the study.
id UERJ-21_8a6a58fc1ad72417388008241aecd2b1
oai_identifier_str oai:ojs.www.e-publicacoes.uerj.br:article/40947
network_acronym_str UERJ-21
network_name_str Geo UERJ
repository_id_str
spelling ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASILTHERMAL INDEXES FOR THE IDENTIFICATION OF HEAT WAVES APPLIED TO STATE OF PARANÁ, BRAZIL.extremos térmicos. Índices. ondas de calor. Paranáthermal extremes. Indices. heat waves. ParanáThe purpose of this work is to analyze the variability of the maximum annual temperatures in the state of Paraná from 1976 to 2015 to identify the occurrence of periods of extreme heat. Two different indexes were applied: 1) spring - summer (P - V) and 2) daily index (ID). The P-V index allows you to detect only the most extreme events. It was found that they occur more frequently in the months of November to February. The ID index identifies the anomalous warming events that occur throughout the year. It was found that the largest records occur in the autumn and winter seasons. Analyzing both indices it was possible to discover that the stations located in the northern and western regions of Paraná, mainly those located north of the Tropic of Capricorn, presented more significant heat waves, with longer duration and with higher temperatures. On the other hand, the stations located in the center-south registered heat waves with less intensity and duration. Due to the fact that the heat waves are characterized in different ways by the applied methods, the results are dependent on the index used, so the selection of the criterion to determine the heat waves depends on the purpose of the study.The purpose of this work is to analyze the variability of the maximum annual temperatures in the state of Paraná from 1976 to 2015 to identify the occurrence of periods of extreme heat. Two different indexes were applied: 1) spring - summer (P - V) and 2) daily index (ID). The P-V index allows you to detect only the most extreme events. It was found that they occur more frequently in the months of November to February. The ID index identifies the anomalous warming events that occur throughout the year. It was found that the largest records occur in the autumn and winter seasons. Analyzing both indices it was possible to discover that the stations located in the northern and western regions of Paraná, mainly those located north of the Tropic of Capricorn, presented more significant heat waves, with longer duration and with higher temperatures. On the other hand, the stations located in the center-south registered heat waves with less intensity and duration. Due to the fact that the heat waves are characterized in different ways by the applied methods, the results are dependent on the index used, so the selection of the criterion to determine the heat waves depends on the purpose of the study.O objetivo do presente estudo foi produzir uma análise da variabilidade das temperaturas máximas anuais no estado do Paraná no período de 1976 a 2015 para identificar a ocorrência de períodos de extremos de calor. Para tanto foram aplicados dois diferentes índices: 1) primavera – verão (P-V) e 2) índice diário (ID). O índice P-V permite detectar somente os eventos mais extremos e, no Paraná, foi verificado que estes ocorrem com maior frequência nos meses de novembro a fevereiro. O índice ID identifica os eventos de aquecimento anômalo que ocorrem durante todo o ano e foi constatado que os maiores registros ocorrem nas estações de outono e inverno. Por meio da análise de tais índices foi possível identificar que as estações localizadas na região norte e oeste do estado, principalmente aquelas localizadas ao norte do trópico de Capricórnio, apresentaram ondas de calor mais significativas, de maior duração e com temperaturas mais elevadas. Por outro lado, as estações situadas no centro-sul registraram ondas de calor com menor intensidade e duração. Em virtude do fato das ondas de calor serem caracterizadas de formas diferentes pelos métodos aplicados, destaca-se que os resultados são dependentes do índice utilizado, sendo assim, a seleção do critério para determinar as ondas de calor depende do propósito do estudo.Universidade do Estado do Rio de Janeiro2019-04-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://www.e-publicacoes.uerj.br/geouerj/article/view/4094710.12957/geouerj.2019.40947Geo UERJ; n. 34 (2019): Jan/Jun - Dossiê de Climatologia da ABClima; e409471981-90211415-7543reponame:Geo UERJinstname:Universidade do Estado do Rio de Janeiro (UERJ)instacron:UERJporhttps://www.e-publicacoes.uerj.br/geouerj/article/view/40947/28455Copyright (c) 2019 Deise Fabiana Ely, Karitha Campos Kogimainfo:eu-repo/semantics/openAccessEly, Deise FabianaKogima, Karitha Campos2022-02-20T22:08:37Zoai:ojs.www.e-publicacoes.uerj.br:article/40947Revistahttps://www.e-publicacoes.uerj.br/index.php/geouerjPUBhttps://www.e-publicacoes.uerj.br/index.php/geouerj/oaitunesregina@gmail.com || ppeuerj@eduerj.uerj.br || geouerj.revista@gmail.com || glauciomarafon@hotmail.com1981-90211415-7543opendoar:2022-02-20T22:08:37Geo UERJ - Universidade do Estado do Rio de Janeiro (UERJ)false
dc.title.none.fl_str_mv ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
THERMAL INDEXES FOR THE IDENTIFICATION OF HEAT WAVES APPLIED TO STATE OF PARANÁ, BRAZIL.
title ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
spellingShingle ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
Ely, Deise Fabiana
extremos térmicos. Índices. ondas de calor. Paraná
thermal extremes. Indices. heat waves. Paraná
title_short ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
title_full ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
title_fullStr ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
title_full_unstemmed ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
title_sort ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
author Ely, Deise Fabiana
author_facet Ely, Deise Fabiana
Kogima, Karitha Campos
author_role author
author2 Kogima, Karitha Campos
author2_role author
dc.contributor.author.fl_str_mv Ely, Deise Fabiana
Kogima, Karitha Campos
dc.subject.por.fl_str_mv extremos térmicos. Índices. ondas de calor. Paraná
thermal extremes. Indices. heat waves. Paraná
topic extremos térmicos. Índices. ondas de calor. Paraná
thermal extremes. Indices. heat waves. Paraná
description The purpose of this work is to analyze the variability of the maximum annual temperatures in the state of Paraná from 1976 to 2015 to identify the occurrence of periods of extreme heat. Two different indexes were applied: 1) spring - summer (P - V) and 2) daily index (ID). The P-V index allows you to detect only the most extreme events. It was found that they occur more frequently in the months of November to February. The ID index identifies the anomalous warming events that occur throughout the year. It was found that the largest records occur in the autumn and winter seasons. Analyzing both indices it was possible to discover that the stations located in the northern and western regions of Paraná, mainly those located north of the Tropic of Capricorn, presented more significant heat waves, with longer duration and with higher temperatures. On the other hand, the stations located in the center-south registered heat waves with less intensity and duration. Due to the fact that the heat waves are characterized in different ways by the applied methods, the results are dependent on the index used, so the selection of the criterion to determine the heat waves depends on the purpose of the study.The purpose of this work is to analyze the variability of the maximum annual temperatures in the state of Paraná from 1976 to 2015 to identify the occurrence of periods of extreme heat. Two different indexes were applied: 1) spring - summer (P - V) and 2) daily index (ID). The P-V index allows you to detect only the most extreme events. It was found that they occur more frequently in the months of November to February. The ID index identifies the anomalous warming events that occur throughout the year. It was found that the largest records occur in the autumn and winter seasons. Analyzing both indices it was possible to discover that the stations located in the northern and western regions of Paraná, mainly those located north of the Tropic of Capricorn, presented more significant heat waves, with longer duration and with higher temperatures. On the other hand, the stations located in the center-south registered heat waves with less intensity and duration. Due to the fact that the heat waves are characterized in different ways by the applied methods, the results are dependent on the index used, so the selection of the criterion to determine the heat waves depends on the purpose of the study.
publishDate 2019
dc.date.none.fl_str_mv 2019-04-15
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://www.e-publicacoes.uerj.br/geouerj/article/view/40947
10.12957/geouerj.2019.40947
url https://www.e-publicacoes.uerj.br/geouerj/article/view/40947
identifier_str_mv 10.12957/geouerj.2019.40947
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://www.e-publicacoes.uerj.br/geouerj/article/view/40947/28455
dc.rights.driver.fl_str_mv Copyright (c) 2019 Deise Fabiana Ely, Karitha Campos Kogima
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2019 Deise Fabiana Ely, Karitha Campos Kogima
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade do Estado do Rio de Janeiro
publisher.none.fl_str_mv Universidade do Estado do Rio de Janeiro
dc.source.none.fl_str_mv Geo UERJ; n. 34 (2019): Jan/Jun - Dossiê de Climatologia da ABClima; e40947
1981-9021
1415-7543
reponame:Geo UERJ
instname:Universidade do Estado do Rio de Janeiro (UERJ)
instacron:UERJ
instname_str Universidade do Estado do Rio de Janeiro (UERJ)
instacron_str UERJ
institution UERJ
reponame_str Geo UERJ
collection Geo UERJ
repository.name.fl_str_mv Geo UERJ - Universidade do Estado do Rio de Janeiro (UERJ)
repository.mail.fl_str_mv tunesregina@gmail.com || ppeuerj@eduerj.uerj.br || geouerj.revista@gmail.com || glauciomarafon@hotmail.com
_version_ 1799317529583157248