A Study of the Phenomenon of Urban Heat Island in Rio de Janeiro Metropolitan Region
Autor(a) principal: | |
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Data de Publicação: | 2017 |
Outros Autores: | , |
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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Anuário do Instituto de Geociências (Online) |
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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 |
|
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/7833 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 |
language |
por |
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 |
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 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) instname:Universidade Federal do Rio de Janeiro (UFRJ) instacron:UFRJ |
instname_str |
Universidade Federal do Rio de Janeiro (UFRJ) |
instacron_str |
UFRJ |
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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1797053544525725696 |