THE INTENSITY OF SURFACE HEAT ISLANDS AND THE VEGETATION INDEX USING NORMALIZED DIFFERENCE IN RONDONOPOLIS-MT

Registro completo de metadados
MetadadosDescriçãoIdioma
Autor(es): dc.contributorRede Estadual Ensino Estado Mato Grosso-
Autor(es): dc.contributorUniversidade Estadual Paulista (UNESP)-
Autor(es): dc.creatorGomes, Washington Paulo-
Autor(es): dc.creatorCosta Trindade Amorim, Margarete Cristiane de-
Data de aceite: dc.date.accessioned2025-08-21T18:16:22Z-
Data de disponibilização: dc.date.available2025-08-21T18:16:22Z-
Data de envio: dc.date.issued2025-04-29-
Data de envio: dc.date.issued2023-12-31-
Fonte completa do material: dc.identifierhttps://hdl.handle.net/11449/297300-
Fonte: dc.identifier.urihttp://educapes.capes.gov.br/handle/11449/297300-
Descrição: dc.descriptionThe utilization of thermal infrared sensor via satellite imagery represents a significant technique for intra-urban temperatures, aiding in understanding the formation of surface heat islands within spatial context, considering Earth's utilization and occupation. Remote sensors for surface temperature detection offer advantages, providing frequent data on the Earth's surface and facilitating the examination of urban thermal environment across various spatial and temporal scales. This study aimed to analyze the intensity of surface heat islands during four episodes spanning the dry and rainy seasons in Rondonopolis-MT. To achieve this, images from the Landsat 8 satellite, utilizing the thermal infrared channel/TIRS 1 (band 10), were employed to identify heat islands, while the red channels (band 4) and near-infrared (band 5) were utilised to assess vegetation levels via the Normalized Difference Vegetation Index (NDVI). The findings revealed that surfacel heat islands exhibited strong magnitudes, reaching intensities of up to 14 degrees C. During the dry season, intensities were heightened due to fires, leading to increased surface absorption capacity, attributed to a combination of factors including greater soil exposure, heightened radiation absorption by carbonized vegetation, and reduced evapotranspiration.-
Descrição: dc.descriptionRede Estadual Ensino Estado Mato Grosso, Cuiaba, Brazil-
Descrição: dc.descriptionUniv Estadual Paulista, Fac Ciencias Tecnol, Dept Geog, Campus Presidente Prudente, Presidente Prudente, Brazil-
Descrição: dc.descriptionUniv Estadual Paulista, Fac Ciencias Tecnol, Dept Geog, Campus Presidente Prudente, Presidente Prudente, Brazil-
Formato: dc.format25-
Idioma: dc.languagept_BR-
Publicador: dc.publisherUniv Estadual Paulista Julio Mesquita Filho-
Relação: dc.relationRevista Formacao Online-
???dc.source???: dc.sourceWeb of Science-
Palavras-chave: dc.subjectSurface Heat Island-
Palavras-chave: dc.subjectVegetation Index-
Palavras-chave: dc.subjectRondonopolis-MT-
Título: dc.titleTHE INTENSITY OF SURFACE HEAT ISLANDS AND THE VEGETATION INDEX USING NORMALIZED DIFFERENCE IN RONDONOPOLIS-MT-
Tipo de arquivo: dc.typelivro digital-
Aparece nas coleções:Repositório Institucional - Unesp

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