ÍNDICES TÉRMICOS PARA A IDENTIFICAÇÃO DE ONDAS DE CALOR APLICADOS AO ESTADO DO PARANÁ, BRASIL
Autor(a) principal: | |
---|---|
Data de Publicação: | 2019 |
Outros Autores: | |
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 |