Land cover and socioeconomic vulnerability is associated with unequal warming in a hyper-arid city in Northwest Mexico

Read full text
Authors: Eric Sigala-Meza, Francisco José Del-Toro-Guerrero, Stephen Holmes Bullock, I. Zavala-Guillén, Rodrigo Méndez-Alonzo
Cited by: 2
References: 66

Abstract

Urban expansion and land cover change can intensify the effects of urban heat islands (UHIs). While previous studies have associated UHI intensity with land cover patterns, the causal links to socioeconomic factors are less frequently explored, particularly in extreme environments. In this study, we used Landsat 5, 7, and 8 Imagery between 1991 and 2023 to characterize the evolution of the Surface Urban Heat Island (SUHI) and tested how Land Surface Temperatures (LST) are associated with land cover patterns and socioeconomic variability within Mexicali, one of the cities with the hottest temperature records in North America. We found significant long-term trends in LST with an average increase of approximately 0.15 °C per year, with a SUHI that peaks in April at 4.59 °C, large seasonal variation, and a strong correlation with available weather station data. By analyzing spatially explicit patterns of SUHI, in relation to green infrastructure coverage across 429 socioeconomic sub-municipal areas for years 2018–2022, we developed an integrative Urban Heat Vulnerability Index (UHVI) which identified areas where lower socioeconomic marginalization coincides with more green coverage and lower LST. In contrast, the most socioeconomically marginalized areas were subject to higher temperatures and less vegetation. Our results indicate that Mexicali is a vegetation-deprived city in need of transformative changes to reduce urban heat, particularly in peripheral, lower-income neighborhoods. We recommend implementing nature-based solutions such as drought-tolerant urban greening and green roofs to mitigate the impacts of extreme heat in one of the hottest cities in North America. • We quantified the Urban Heat Island of Mexicali, México, from 1991 to 2023. • Land Surface Temperatures increased ∼ 0.15 °C per year and SUHI peaked at 4.6 °C. • Bare soil LST was ∼2.5 °C hotter than built-up areas and ∼ 5 °C hotter than vegetation. • We combined LST, socioeconomic and vegetation data into a heat vulnerability index. • Socially deprived neighborhoods had higher mean LST and lower vegetation.

Fields of Study & Subjects

Urban Heat Island Mitigation Climate change impacts on agriculture Remote Sensing in Agriculture

Publication details

Journal / source
Urban Climate
Publisher
Elsevier BV
Volume
66
Pages
102842–102842
Publication date
1 March 2026
Language
EN