TY - JOUR
T1 - Superficial Urban Heat Island in the City of Santos, Brazil
AU - Angeles Suazo, Julio
AU - Angeles Vasquez, Roberto
AU - Lavado Meza, Carmencita
AU - Angeles Suazo, Nataly
AU - de la Cruz Cerrón, Leonel
AU - Meza Mitma, Pabel
AU - Flores Rojas, Jose
AU - Abi Karam, Hugo
N1 - Publisher Copyright:
© 2025 by the authors.
PY - 2025/12
Y1 - 2025/12
N2 - This contribution estimates the intensity of Urban Heat Island (UHI) during the period 2001-2020 for the city of Santos (CS), located in São Paulo, Brazil. The formation of the Surface Urban Heat Island (SUHI) was quantified from 2 methods: the first was Streutker’s method, which adjusts the surface soil temperature (LST) (urban and rural surface) to a Gaussian surface. The second, the quantile method proposed by Jose Flores, uses the difference between the 0.95 quantile of the LST of the urban area and the median of the LST of the rural area. Both methods use remote sensing data of LST at 0.05° resolution, obtained from the MODIS sensor on board the TERRA and AQUA satellites. In general, the quantile method can be used as a complementary analysis to the Streutker method for cities with high LST. The results of the CS analysis, during diurnal periods, indicate maximum values in May (5.09°C) and minimum values in August (3.87°C). During the night period, it presented maximum values in February (3.94°C) and minimum values in August (2.40°C) with the quantile method, and due to its proximity to the Small Ocean, the Streutker method presents interferences.
AB - This contribution estimates the intensity of Urban Heat Island (UHI) during the period 2001-2020 for the city of Santos (CS), located in São Paulo, Brazil. The formation of the Surface Urban Heat Island (SUHI) was quantified from 2 methods: the first was Streutker’s method, which adjusts the surface soil temperature (LST) (urban and rural surface) to a Gaussian surface. The second, the quantile method proposed by Jose Flores, uses the difference between the 0.95 quantile of the LST of the urban area and the median of the LST of the rural area. Both methods use remote sensing data of LST at 0.05° resolution, obtained from the MODIS sensor on board the TERRA and AQUA satellites. In general, the quantile method can be used as a complementary analysis to the Streutker method for cities with high LST. The results of the CS analysis, during diurnal periods, indicate maximum values in May (5.09°C) and minimum values in August (3.87°C). During the night period, it presented maximum values in February (3.94°C) and minimum values in August (2.40°C) with the quantile method, and due to its proximity to the Small Ocean, the Streutker method presents interferences.
KW - Land surface temperature
KW - Quantiles method
KW - Streutker method
KW - Urban climatology
KW - Urban heat island in Santos
KW - Urban-rural temperature contrast
UR - https://www.scopus.com/pages/publications/105024139948
U2 - 10.46488/NEPT.2025.v24i04.D1776
DO - 10.46488/NEPT.2025.v24i04.D1776
M3 - Original Article
AN - SCOPUS:105024139948
SN - 0972-6268
VL - 24
JO - Nature Environment and Pollution Technology
JF - Nature Environment and Pollution Technology
IS - 4
M1 - D1776
ER -