A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region

Detalhes bibliográficos
Autor(a) principal: Meireles, Victor Hugo Pezzini de
Data de Publicação: 2017
Outros Autores: França, José Ricardo de Almeida, Peres, Leonardo F.
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/7833
Resumo: The main objective of this study is analyze the field of Surface Temperature (TS) of the Metropolitan Region of Rio de Janeiro (RMRJ) and its relation to land use. The analysis was based on vegetation index NDVI and TS values obtained from NOAA - 14 and 18 images covering the 2005 to 2010 years. The Maximum Value Composite method was used to generate of TS and NDVI monthly maps and also for all data period. The different statistical parameters (e.g. correlation and determination coefficients, linear regression and standard deviation) were calculated to determine the relationship between TS and NDVI. The TS monthly values for NOAA - 14 satellite shown to be high in the early morning, although slightly lower than NOAA - 18 satellite due to the different times of passage. It was observed that Urban Heat Island (ICU) phenomenon operates throughout the year, especially in the eastern portion of the city and in the Baixada Fluminense cities. The inverse relationship between TS and NDVI was observed mainly in the autumn and winter months with the highest correlation and determination coefficients. However, this is not observed in the summer months because the heating effect of macroscale (weather effects) overlaps with land use.
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spelling A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan RegionUm Estudo do Fenômeno da Ilha de Calor Urbana na Região Metropolitana do Rio de Janeiro (RMRJ)Urban Heat; RMRJ; NOAA -- 14 and 18 satellites.Ilha de Calor Urbana; RMRJ; Satélites NOAA -- 14 e 18.The main objective of this study is analyze the field of Surface Temperature (TS) of the Metropolitan Region of Rio de Janeiro (RMRJ) and its relation to land use. The analysis was based on vegetation index NDVI and TS values obtained from NOAA - 14 and 18 images covering the 2005 to 2010 years. The Maximum Value Composite method was used to generate of TS and NDVI monthly maps and also for all data period. The different statistical parameters (e.g. correlation and determination coefficients, linear regression and standard deviation) were calculated to determine the relationship between TS and NDVI. The TS monthly values for NOAA - 14 satellite shown to be high in the early morning, although slightly lower than NOAA - 18 satellite due to the different times of passage. It was observed that Urban Heat Island (ICU) phenomenon operates throughout the year, especially in the eastern portion of the city and in the Baixada Fluminense cities. The inverse relationship between TS and NDVI was observed mainly in the autumn and winter months with the highest correlation and determination coefficients. However, this is not observed in the summer months because the heating effect of macroscale (weather effects) overlaps with land use.O principal objetivo deste estudo é analisar o campo de temperatura da superfície (TS) da Região Metropolitana do Rio de Rio de Janeiro (RMRJ) e sua relação com o uso do solo. A análise foi realizada com base no índice de vegetação NDVI e em valores de TS obtidos a partir de imagens dos satélites NOAA - 14 e 18 cobrindo os anos de 2005 a 2010. O método de Composição de Máximo Valor foi utilizado para gerar mapas mensais de TS e NDVI, e também, para todo o período dos dados. Diferentes parâmetros estatísticos (e.g., coeficientes de correlação e determinação, regressão linear e desvio-padrão) foram calculados para determinar a relação entre TS e NDVI. Os valores mensais de TS para o satélite NOAA - 14 mostraram-se elevados no início da manhã, apesar de serem ligeiramente inferiores ao NOAA - 18 devido aos diferentes horários de passagem. Observou-se que o fenômeno da Ilha de Calor Urbana (ICU) atua ao longo do ano, principalmente na porção leste da cidade e em municípios da Baixada Fluminense. A relação inversa entre TS e NDVI foi evidenciada principalmente nos meses de outono e inverno com os maiores coeficientes de correlação e determinação. Porém, tal fato não é verificado no verão, pois o efeito do aquecimento de macroescala (efeitos meteorológicos) se sobrepõe ao uso do solo.Universidade Federal do Rio de Janeiro2017-02-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/783310.11137/2014_2_180_194Anuário do Instituto de Geociências; Vol 37, No 2 (2014); 180-194Anuário do Instituto de Geociências; Vol 37, No 2 (2014); 180-1941982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/7833/6314Copyright (c) 2014 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessMeireles, Victor Hugo Pezzini deFrança, José Ricardo de AlmeidaPeres, Leonardo F.2017-02-15T17:28:22Zoai:www.revistas.ufrj.br:article/7833Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-02-15T17:28:22Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
Um Estudo do Fenômeno da Ilha de Calor Urbana na Região Metropolitana do Rio de Janeiro (RMRJ)
title A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
spellingShingle A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
Meireles, Victor Hugo Pezzini de
Urban Heat; RMRJ; NOAA -- 14 and 18 satellites.
Ilha de Calor Urbana; RMRJ; Satélites NOAA -- 14 e 18.
title_short A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
title_full A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
title_fullStr A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
title_full_unstemmed A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
title_sort A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
author Meireles, Victor Hugo Pezzini de
author_facet Meireles, Victor Hugo Pezzini de
França, José Ricardo de Almeida
Peres, Leonardo F.
author_role author
author2 França, José Ricardo de Almeida
Peres, Leonardo F.
author2_role author
author
dc.contributor.author.fl_str_mv Meireles, Victor Hugo Pezzini de
França, José Ricardo de Almeida
Peres, Leonardo F.
dc.subject.por.fl_str_mv Urban Heat; RMRJ; NOAA -- 14 and 18 satellites.
Ilha de Calor Urbana; RMRJ; Satélites NOAA -- 14 e 18.
topic Urban Heat; RMRJ; NOAA -- 14 and 18 satellites.
Ilha de Calor Urbana; RMRJ; Satélites NOAA -- 14 e 18.
description The main objective of this study is analyze the field of Surface Temperature (TS) of the Metropolitan Region of Rio de Janeiro (RMRJ) and its relation to land use. The analysis was based on vegetation index NDVI and TS values obtained from NOAA - 14 and 18 images covering the 2005 to 2010 years. The Maximum Value Composite method was used to generate of TS and NDVI monthly maps and also for all data period. The different statistical parameters (e.g. correlation and determination coefficients, linear regression and standard deviation) were calculated to determine the relationship between TS and NDVI. The TS monthly values for NOAA - 14 satellite shown to be high in the early morning, although slightly lower than NOAA - 18 satellite due to the different times of passage. It was observed that Urban Heat Island (ICU) phenomenon operates throughout the year, especially in the eastern portion of the city and in the Baixada Fluminense cities. The inverse relationship between TS and NDVI was observed mainly in the autumn and winter months with the highest correlation and determination coefficients. However, this is not observed in the summer months because the heating effect of macroscale (weather effects) overlaps with land use.
publishDate 2017
dc.date.none.fl_str_mv 2017-02-15
dc.type.none.fl_str_mv

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10.11137/2014_2_180_194
url https://revistas.ufrj.br/index.php/aigeo/article/view/7833
identifier_str_mv 10.11137/2014_2_180_194
dc.language.iso.fl_str_mv por
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dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/7833/6314
dc.rights.driver.fl_str_mv Copyright (c) 2014 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2014 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
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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 37, No 2 (2014); 180-194
Anuário do Instituto de Geociências; Vol 37, No 2 (2014); 180-194
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
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