Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico

Climate change has severe consequences on ecosystem processes, as well as on people’s quality of life. It has been suggested that the loss of vegetation cover increases the land surface temperature (LST) due to modifications in biogeochemical patterns, generating a phenomenon known as “urban heat island” (UHI). The aim of this work was to analyze the effects of urban land-cover changes on the spatiotemporal variation of surface temperature in the tropical city of Mérida, Mexico. To find these effects we used both detected land-cover changes as well as variations of the Normalized Difference Vegetation Index (NDVI). Mérida is ranked worldwide as one of the best cities to live due to its quality of life. Data from satellite images of Landsat were analyzed to calculate land use change (LUC), LST, and NDVI. LST increased ca. 4 °C in the dry season and 3 °C in the wet season because of the LUC. In addition, a positive relationship between the LST and the NDVI was observed mainly in the dry season. The results confirm an increase in the LST as a consequence of the loss of vegetation cover, which favors the urban heat island phenomenon.

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Main Authors: Palafox Juárez, Jorge Omar López_Martínez, JOSE LUIS HERNANDEZ STEFANONI, Héctor Hernández Núñez
Format: info:eu-repo/semantics/article biblioteca
Language:eng
Subjects:info:eu-repo/classification/Autores/URBAN HEAT ISLAND, info:eu-repo/classification/Autores/LAND USE CHANGE, info:eu-repo/classification/Autores/REMOTE SENSING, info:eu-repo/classification/Autores/LANDSAT SENSOR, info:eu-repo/classification/cti/2, info:eu-repo/classification/cti/24, info:eu-repo/classification/cti/2417, info:eu-repo/classification/cti/241713,
Online Access:http://cicy.repositorioinstitucional.mx/jspui/handle/1003/2086
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spelling dig-cicy-1003-20862022-08-31T13:45:12Z Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico Palafox Juárez Jorge Omar López_Martínez JOSE LUIS HERNANDEZ STEFANONI Héctor Hernández Núñez 2021 info:eu-repo/semantics/article Climate change has severe consequences on ecosystem processes, as well as on people’s quality of life. It has been suggested that the loss of vegetation cover increases the land surface temperature (LST) due to modifications in biogeochemical patterns, generating a phenomenon known as “urban heat island” (UHI). The aim of this work was to analyze the effects of urban land-cover changes on the spatiotemporal variation of surface temperature in the tropical city of Mérida, Mexico. To find these effects we used both detected land-cover changes as well as variations of the Normalized Difference Vegetation Index (NDVI). Mérida is ranked worldwide as one of the best cities to live due to its quality of life. Data from satellite images of Landsat were analyzed to calculate land use change (LUC), LST, and NDVI. LST increased ca. 4 °C in the dry season and 3 °C in the wet season because of the LUC. In addition, a positive relationship between the LST and the NDVI was observed mainly in the dry season. The results confirm an increase in the LST as a consequence of the loss of vegetation cover, which favors the urban heat island phenomenon. info:eu-repo/classification/Autores/URBAN HEAT ISLAND info:eu-repo/classification/Autores/LAND USE CHANGE info:eu-repo/classification/Autores/REMOTE SENSING info:eu-repo/classification/Autores/LANDSAT SENSOR info:eu-repo/classification/cti/2 info:eu-repo/classification/cti/24 info:eu-repo/classification/cti/2417 info:eu-repo/classification/cti/241713 info:eu-repo/classification/cti/241713 ISPRS International Journal of Geo-Information, 10(2), 76, 2021. http://cicy.repositorioinstitucional.mx/jspui/handle/1003/2086 info:eu-repo/semantics/datasetDOI/https://doi.org/10.3390/ijgi10020076 info:eu-repo/semantics/openAccess eng citation:Palafox-Juárez, E. B., López-Martínez, J. O., Hernández-Stefanoni, J. L., & Hernández-Nuñez, H. (2021). Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico. ISPRS International Journal of Geo-Information, 10(2), 76. http://creativecommons.org/licenses/by-nc-nd/4.0 info:eu-repo/semantics/publishedVersion application/pdf
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country México
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language eng
topic info:eu-repo/classification/Autores/URBAN HEAT ISLAND
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info:eu-repo/classification/Autores/LANDSAT SENSOR
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spellingShingle info:eu-repo/classification/Autores/URBAN HEAT ISLAND
info:eu-repo/classification/Autores/LAND USE CHANGE
info:eu-repo/classification/Autores/REMOTE SENSING
info:eu-repo/classification/Autores/LANDSAT SENSOR
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info:eu-repo/classification/Autores/URBAN HEAT ISLAND
info:eu-repo/classification/Autores/LAND USE CHANGE
info:eu-repo/classification/Autores/REMOTE SENSING
info:eu-repo/classification/Autores/LANDSAT SENSOR
info:eu-repo/classification/cti/2
info:eu-repo/classification/cti/24
info:eu-repo/classification/cti/2417
info:eu-repo/classification/cti/241713
info:eu-repo/classification/cti/241713
Palafox Juárez
Jorge Omar López_Martínez
JOSE LUIS HERNANDEZ STEFANONI
Héctor Hernández Núñez
Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico
description Climate change has severe consequences on ecosystem processes, as well as on people’s quality of life. It has been suggested that the loss of vegetation cover increases the land surface temperature (LST) due to modifications in biogeochemical patterns, generating a phenomenon known as “urban heat island” (UHI). The aim of this work was to analyze the effects of urban land-cover changes on the spatiotemporal variation of surface temperature in the tropical city of Mérida, Mexico. To find these effects we used both detected land-cover changes as well as variations of the Normalized Difference Vegetation Index (NDVI). Mérida is ranked worldwide as one of the best cities to live due to its quality of life. Data from satellite images of Landsat were analyzed to calculate land use change (LUC), LST, and NDVI. LST increased ca. 4 °C in the dry season and 3 °C in the wet season because of the LUC. In addition, a positive relationship between the LST and the NDVI was observed mainly in the dry season. The results confirm an increase in the LST as a consequence of the loss of vegetation cover, which favors the urban heat island phenomenon.
format info:eu-repo/semantics/article
topic_facet info:eu-repo/classification/Autores/URBAN HEAT ISLAND
info:eu-repo/classification/Autores/LAND USE CHANGE
info:eu-repo/classification/Autores/REMOTE SENSING
info:eu-repo/classification/Autores/LANDSAT SENSOR
info:eu-repo/classification/cti/2
info:eu-repo/classification/cti/24
info:eu-repo/classification/cti/2417
info:eu-repo/classification/cti/241713
info:eu-repo/classification/cti/241713
author Palafox Juárez
Jorge Omar López_Martínez
JOSE LUIS HERNANDEZ STEFANONI
Héctor Hernández Núñez
author_facet Palafox Juárez
Jorge Omar López_Martínez
JOSE LUIS HERNANDEZ STEFANONI
Héctor Hernández Núñez
author_sort Palafox Juárez
title Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico
title_short Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico
title_full Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico
title_fullStr Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico
title_full_unstemmed Impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical City of Mexico
title_sort impact of urban land-cover changes on the spatial-temporal land surface temperature in a tropical city of mexico
url http://cicy.repositorioinstitucional.mx/jspui/handle/1003/2086
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