Abstract

Exposure to heat is a growing public health concern as climate change accelerates worldwide. Different socioeconomic and racial groups often face unequal exposure to heat as well as increased heat-related sickness, mortality, and energy costs. We provide new insight into thermal inequities by analyzing 20 Southwestern U.S. metropolitan regions at the census block group scale for three temperature scenarios (average summer heat, extreme summer heat, and average summer nighttime heat). We first compared average temperatures for top and bottom decile block groups according to demographic variables. Then we used spatial regression models to investigate the extent to which exposure to heat (measured by land surface temperature) varies according to income and race. Large thermal inequities exist within all the regions studied. On average, the poorest 10% of neighborhoods in an urban region were 2.2 °C (4 °F) hotter than the wealthiest 10% on both extreme heat days and average summer days. The difference was as high as 3.3–3.7 °C (6–7 °F) in California metro areas such as Palm Springs and the Inland Empire. A similar pattern held for Latinx neighborhoods. Temperature disparities at night were much smaller (usually ~1 °F). Disparities for Black neighborhoods were also lower, perhaps because Black populations are small in most of these cities. California urban regions show stronger thermal disparities than those in other Southwestern states, perhaps because inexpensive water has led to more extensive vegetation in affluent neighborhoods. Our findings provide new details about urban thermal inequities and reinforce the need for programs to reduce the disproportionate heat experienced by disadvantaged communities.

Highlights

  • Urban heat is a public health hazard that is experienced across the globe independent of jurisdiction, development, and climate

  • We found the poorest 10% of neighborhoods in each region to be about 2.2 ◦ C (4 ◦ F) hotter than the wealthiest on both extreme heat days and average summer days

  • Our in-depth analysis identifies large and consistent variations often 2.2–3.9 °C

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Summary

Introduction

Urban heat is a public health hazard that is experienced across the globe independent of jurisdiction, development, and climate. Extreme heat events exacerbate the impact of urban heat and are responsible for a high number of weather-related deaths [1] Excess heat has consequences for human health including heat stroke, exhaustion, and amplified respiratory and cardiovascular issues [2]. It has long been known that the paved surfaces of urban areas will absorb and retain solar radiation, increasing urban temperatures [3,4]. For this reason, cities in temperate climates will often have higher temperatures than vegetated surrounding countrysides, a phenomenon known as the urban heat island (UHI) effect [5,6]. Particular neighborhoods with high levels of paved surfaces may be hotter than others with more vegetation

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