Version 1
: Received: 1 April 2023 / Approved: 4 April 2023 / Online: 4 April 2023 (12:37:09 CEST)
How to cite:
Fernandes, R.; Ferreira, A.; Nascimento, V.; Freitas, M. Assessment of Urban Heat Island in the Northeastern State Capitals in Brazil Using Sentinel Satellite Data – 3 SLSTR. Preprints2023, 2023040045. https://doi.org/10.20944/preprints202304.0045.v1
Fernandes, R.; Ferreira, A.; Nascimento, V.; Freitas, M. Assessment of Urban Heat Island in the Northeastern State Capitals in Brazil Using Sentinel Satellite Data – 3 SLSTR. Preprints 2023, 2023040045. https://doi.org/10.20944/preprints202304.0045.v1
Fernandes, R.; Ferreira, A.; Nascimento, V.; Freitas, M. Assessment of Urban Heat Island in the Northeastern State Capitals in Brazil Using Sentinel Satellite Data – 3 SLSTR. Preprints2023, 2023040045. https://doi.org/10.20944/preprints202304.0045.v1
APA Style
Fernandes, R., Ferreira, A., Nascimento, V., & Freitas, M. (2023). Assessment of Urban Heat Island in the Northeastern State Capitals in Brazil Using Sentinel Satellite Data – 3 SLSTR. Preprints. https://doi.org/10.20944/preprints202304.0045.v1
Chicago/Turabian Style
Fernandes, R., Victor Nascimento and Marcos Freitas. 2023 "Assessment of Urban Heat Island in the Northeastern State Capitals in Brazil Using Sentinel Satellite Data – 3 SLSTR" Preprints. https://doi.org/10.20944/preprints202304.0045.v1
Abstract
The Surface Urban Heat Island (UHI) is caused by the difference in temperature between the urban and its surrounding areas. However, in the scientific literature, there is no solid methodology defining urban and non-urban areas, which is essential to estimate the SUHI with greater accuracy. This study uses the official national urban areas limit, to obtain the SUHI more accurately on the nine northeastern Brazilian capitals. The land surface temperature was obtained using the Sentinel 3 satellite data for the years 2019 and 2020. Afterward, the maximum and average SUHI, and the complementary indexes were calculated, such as the Urban Thermal Field Variation Index (UTFVI) and the Thermal Discomfort Index (TDI) for the urban areas and their surrounding areas. The Maximum and Average SUHI, obtained values between 1.85 and 8.25 and -4.92 and 2.59 degree difference, respectively, proving the SUHI existence in the study areas. The UTFVI, with values between 0.010 and 0.040, expresses how bad the eco-environmental spaces of urban are. The TDI, with values between 24.61 and 28.89 ºC, expresses the population’s thermal comfort. Therefore, this study provides a better understanding of the surface UHI pioneeringly for the Brazilian Northeast Region.
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
