Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images
Autor(a) principal: | |
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Data de Publicação: | 2022 |
Outros Autores: | , , , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UFRGS |
Texto Completo: | http://hdl.handle.net/10183/246954 |
Resumo: | The inverse correlation between NDVI and LST is widely known for its long time series. However, when more specific statistical tests were performed, subtle differences in the correlation behavior over time are more clearly observed. In this work, regression analyses were performed between NDVI and LST at intervals of approximately 10 years, quantifying this relationship for an area of transition from vegetation to urban occupation from 1985 to 2018. The removal of vegetation cover (reduction of 51% to 7% in grassland and 14.4% to 0.6% in forest) to occupy impermeable surfaces ( increase of 31% to 91% in urban areas) caused an average LST increase of 4.18 °C when compared to the first and last decades of the historical series. Temporal analysis allowed us to verify the increase in temperature in the four seasons. The largest difference was 6.36 °C between the first and last decade of autumn, 4.40 °C in spring, 4.09 °C in summer, and 2.41 °C in winter. The results also show that LST has a negative correlation with NDVI, especially in urban areas, with an increase in this correlation during the period (1989: R = −0.55; 1999: R = −0.58; 2008: R = −0.59; 2018: R = −0.76). Our study results will help policymakers understand the dynamics of temperature increases by adding scientifically relevant information on the sustainable organization of the urban environment. |
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Kaiser, Eduardo AndréRolim, Silvia Beatriz AlvesGrondona, Atilio Efrain BicaHackmann, Cristiano LimaLinn, Rodrigo de MarsillacKäfer, Pâmela SuélenRocha, Nájila Souza daDiaz, Lucas Ribeiro2022-08-16T04:46:59Z20222073-4433http://hdl.handle.net/10183/246954001139625The inverse correlation between NDVI and LST is widely known for its long time series. However, when more specific statistical tests were performed, subtle differences in the correlation behavior over time are more clearly observed. In this work, regression analyses were performed between NDVI and LST at intervals of approximately 10 years, quantifying this relationship for an area of transition from vegetation to urban occupation from 1985 to 2018. The removal of vegetation cover (reduction of 51% to 7% in grassland and 14.4% to 0.6% in forest) to occupy impermeable surfaces ( increase of 31% to 91% in urban areas) caused an average LST increase of 4.18 °C when compared to the first and last decades of the historical series. Temporal analysis allowed us to verify the increase in temperature in the four seasons. The largest difference was 6.36 °C between the first and last decade of autumn, 4.40 °C in spring, 4.09 °C in summer, and 2.41 °C in winter. The results also show that LST has a negative correlation with NDVI, especially in urban areas, with an increase in this correlation during the period (1989: R = −0.55; 1999: R = −0.58; 2008: R = −0.59; 2018: R = −0.76). Our study results will help policymakers understand the dynamics of temperature increases by adding scientifically relevant information on the sustainable organization of the urban environment.application/pdfengAtmosphere. Basel. Vol. 13, n. 3 (2022), Art. 460Modelagem urbanaProcesso de urbanizaçãoMeio ambiente urbanoUso da terraTemperatura de superfícieVegetation and urban modelingLand use and land cover changeLand surface processesPorto Alegre four districtsSpatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS imagesEstrangeiroinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSTEXT001139625.pdf.txt001139625.pdf.txtExtracted Texttext/plain66697http://www.lume.ufrgs.br/bitstream/10183/246954/2/001139625.pdf.txta02f8351c6131a541e087d95e89ccb10MD52ORIGINAL001139625.pdfTexto completo (inglês)application/pdf2418734http://www.lume.ufrgs.br/bitstream/10183/246954/1/001139625.pdf39ecb1b8b5afb0dd255550fe0bb4882cMD5110183/2469542022-08-17 04:48:39.103438oai:www.lume.ufrgs.br:10183/246954Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2022-08-17T07:48:39Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false |
dc.title.pt_BR.fl_str_mv |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
title |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
spellingShingle |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images Kaiser, Eduardo André Modelagem urbana Processo de urbanização Meio ambiente urbano Uso da terra Temperatura de superfície Vegetation and urban modeling Land use and land cover change Land surface processes Porto Alegre four districts |
title_short |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
title_full |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
title_fullStr |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
title_full_unstemmed |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
title_sort |
Spatiotemporal influences of LULC changes on land surface temperature in rapid urbanization area by using Landsat-TM and TIRS images |
author |
Kaiser, Eduardo André |
author_facet |
Kaiser, Eduardo André Rolim, Silvia Beatriz Alves Grondona, Atilio Efrain Bica Hackmann, Cristiano Lima Linn, Rodrigo de Marsillac Käfer, Pâmela Suélen Rocha, Nájila Souza da Diaz, Lucas Ribeiro |
author_role |
author |
author2 |
Rolim, Silvia Beatriz Alves Grondona, Atilio Efrain Bica Hackmann, Cristiano Lima Linn, Rodrigo de Marsillac Käfer, Pâmela Suélen Rocha, Nájila Souza da Diaz, Lucas Ribeiro |
author2_role |
author author author author author author author |
dc.contributor.author.fl_str_mv |
Kaiser, Eduardo André Rolim, Silvia Beatriz Alves Grondona, Atilio Efrain Bica Hackmann, Cristiano Lima Linn, Rodrigo de Marsillac Käfer, Pâmela Suélen Rocha, Nájila Souza da Diaz, Lucas Ribeiro |
dc.subject.por.fl_str_mv |
Modelagem urbana Processo de urbanização Meio ambiente urbano Uso da terra Temperatura de superfície |
topic |
Modelagem urbana Processo de urbanização Meio ambiente urbano Uso da terra Temperatura de superfície Vegetation and urban modeling Land use and land cover change Land surface processes Porto Alegre four districts |
dc.subject.eng.fl_str_mv |
Vegetation and urban modeling Land use and land cover change Land surface processes Porto Alegre four districts |
description |
The inverse correlation between NDVI and LST is widely known for its long time series. However, when more specific statistical tests were performed, subtle differences in the correlation behavior over time are more clearly observed. In this work, regression analyses were performed between NDVI and LST at intervals of approximately 10 years, quantifying this relationship for an area of transition from vegetation to urban occupation from 1985 to 2018. The removal of vegetation cover (reduction of 51% to 7% in grassland and 14.4% to 0.6% in forest) to occupy impermeable surfaces ( increase of 31% to 91% in urban areas) caused an average LST increase of 4.18 °C when compared to the first and last decades of the historical series. Temporal analysis allowed us to verify the increase in temperature in the four seasons. The largest difference was 6.36 °C between the first and last decade of autumn, 4.40 °C in spring, 4.09 °C in summer, and 2.41 °C in winter. The results also show that LST has a negative correlation with NDVI, especially in urban areas, with an increase in this correlation during the period (1989: R = −0.55; 1999: R = −0.58; 2008: R = −0.59; 2018: R = −0.76). Our study results will help policymakers understand the dynamics of temperature increases by adding scientifically relevant information on the sustainable organization of the urban environment. |
publishDate |
2022 |
dc.date.accessioned.fl_str_mv |
2022-08-16T04:46:59Z |
dc.date.issued.fl_str_mv |
2022 |
dc.type.driver.fl_str_mv |
Estrangeiro info:eu-repo/semantics/article |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10183/246954 |
dc.identifier.issn.pt_BR.fl_str_mv |
2073-4433 |
dc.identifier.nrb.pt_BR.fl_str_mv |
001139625 |
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2073-4433 001139625 |
url |
http://hdl.handle.net/10183/246954 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartof.pt_BR.fl_str_mv |
Atmosphere. Basel. Vol. 13, n. 3 (2022), Art. 460 |
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info:eu-repo/semantics/openAccess |
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openAccess |
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