Remote sensing applied to biophysical parameters and land cover to identify urban heat islands in Recife (PE), Brazil

Haylla Rebeka de Albuquerque Lins Leonardo; Débora Natália Oliveira de Almeida; Alessandro Rodrigues de Amorim; Anderson Luiz Ribeiro de Paiva; Leidjane Maria Maciel de Oliveira; Sylvana Melo dos Santos

doi:10.5327/Z2176-94782107

Autores

Haylla Rebeka de Albuquerque Lins Leonardo Universidade Federal de Pernambuco (UFPE) - Brasil https://orcid.org/0000-0001-6404-3366
Debora Natália Oliveira de Almeida Universidade Federal de Pernambuco (UFPE) - Brasil https://orcid.org/0000-0001-6000-6138
Alessandro Rodrigues de Amorim Universidade Federal de Pernambuco (UFPE) - Brasil https://orcid.org/0009-0001-2839-8036
Anderson Luiz Ribeiro de Paiva Universidade Federal de Pernambuco (UFPE) - Brasil https://orcid.org/0000-0003-3475-1454
Leidjane Maria Maciel de Oliveira Universidade Federal de Pernambuco (UFPE) - Brasil https://orcid.org/0000-0003-1251-6998
Sylvana Melo dos Santos Universidade Federal de Pernambuco (UFPE) - Brasil https://orcid.org/0000-0003-3106-5301

DOI:

https://doi.org/10.5327/Z2176-94782107

Palavras-chave:

Built-Up Index; índices biofísicos; Google Earth Engine.

Resumo

Do crescimento urbanístico resultam diversas alterações relacionadas, principalmente, com aspectos demográficos, sociais, econômicos e ambientais, decorrendo em uma nova conotação no uso e ocupação do solo. Esse novo cenário impacta o balanço energético local, gerando, como é conhecida, uma “ilha de calor urbana”. Esta pesquisa objetiva investigar a ocorrência de ilhas de calor urbana na cidade do Recife, capital de Pernambuco, Brasil, a partir do processamento de parâmetros biofísicos, da classificação do uso e ocupação do solo e da temperatura da superfície. As imagens orbitais da região de estudo foram obtidas e processadas utilizando-se a plataforma de processamento em nuvem Google Earth Engine, para o período de 2013 a 2021. Os resultados evidenciaram a ocorrência de um aumento das áreas com maior densidade urbana e uma redução das áreas com vegetação. Constatou-se que nas regiões com maior densidade urbana, a temperatura de superfície observada foi até 5,20°C mais elevada do que na área com vegetação.

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