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March 6, 2026Urban Climate2 citationsOpen Access

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

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ESEric Sigala-MezaCenter for Scientific Research and Higher Education at EnsenadaFDFrancisco José Del-Toro-GuerreroUniversidad Autónoma de Baja CaliforniaSBStephen Holmes BullockCenter for Scientific Research and Higher Education at Ensenada

Key Points

  • This research aims to explore the relationship between urban heat islands, land cover, and socioeconomic factors in Mexicali.
  • Analyzed Landsat imagery from 1991 to 2023 to study land cover changes and surface temperatures.
  • Developed an Urban Heat Vulnerability Index (UHVI) based on land surface temperatures and socioeconomic data.
  • Examined the spatial correlation between urban heat and green infrastructure across 429 socioeconomic sub-municipal areas.
  • Average land surface temperatures increased by approximately 0.15 °C per year from 1991 to 2023.
  • The Surface Urban Heat Island (SUHI) peaked at 4.6 °C in April.
  • Bare soil had surface temperatures approximately 2.5 °C hotter than built-up areas and 5 °C hotter than vegetation.
  • Lower socioeconomic areas had higher mean temperatures and less vegetation, indicating greater vulnerability to heat.

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.

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Cite This Study

Sigala-Meza et al. (2026) studied this question.

synapsesocial.com/papers/69aa6f3c531e4c4a9ff594b2https://doi.org/10.1016/j.uclim.2026.102842
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