Las Vegas and Reno have ranked among the two fastest-warming cities in the entire country for years running. The reason isn’t just global climate change. It’s what pavement and concrete do to a desert once you build a city on top of it.
Climate Central, a nonpartisan nonprofit made up of climate scientists, analyzes average annual temperature trends in 242 U.S. cities using open federal data from the National Oceanic and Atmospheric Administration. Its most recent Earth Day analysis found Las Vegas has warmed by roughly 6 degrees Fahrenheit since 1970, placing it second nationally behind Reno, which has warmed by nearly 8 degrees over the same period. Nationally, the contiguous United States has warmed by about 2.8 degrees since 1970, meaning both Nevada cities are heating up at more than twice the national average rate.


Two Different Kinds of Heat, Stacked Together Climate Central ties the underlying national trend directly to rising concentrations of heat-trapping greenhouse gases, largely from burning fossil fuels for energy, transportation, and buildings. But researchers at UNLV point to a second, local factor layered on top of that global trend: the urban heat island effect. Thick layers of pavement and limited green space across the Las Vegas Valley absorb heat during the day and release it slowly overnight, causing Harry Reid International Airport to average five to 15 degrees warmer than the surrounding rural desert on clear nights, according to UNLV research.
Ben Leffel, a UNLV public policy professor who studies climate change, has described the compounding effect in blunt terms: car dependence combined with the valley’s extensive concrete and asphalt footprint is turning the region into an oven. That framing captures why Las Vegas’s warming trend outpaces the broader Southwest, a region Climate Central identifies as warming faster during spring than any other part of the country, averaging 3.4 degrees of additional spring warming.


Why This Matters Beyond Comfort The distinction between global warming and the local urban heat island effect matters because they respond to different solutions on different timelines. The global trend, driven by atmospheric greenhouse gas concentration, only shifts in response to changes in worldwide emissions over years and decades. The local heat island effect, by contrast, responds directly to decisions a city makes about tree canopy, shade structures, reflective building materials, and how much of a neighborhood gets paved over. Cities across Nevada have been expanding tree canopy, adding shade in public spaces, and designating cooling centers specifically to address the piece of the problem that is within local control.
Nearly every one of the 242 U.S. cities Climate Central studied has warmed since the first Earth Day in 1970, and virtually all of that warming traces back to the same global mechanism. What sets Las Vegas apart is the second layer stacked on top of it: a fast-growing desert city whose own built environment amplifies a global trend that residents did not create locally, but now have to live inside every summer.
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