Elisabeth Moyer explains how long-predicted effects of fossil-fuel burning are now manifesting: overall warming that is more uniform (nights and winters warm faster), heavier but less frequent precipitation events, and increased wildfire risk as vegetation dries. Warmer air holds more moisture, driving intense downpours and longer dry spells between storms, while ocean thermal expansion guarantees some degree of sea level rise. Rapid change threatens infrastructure for billions, so coordinated adaptation and mitigation are urgent.
Warm Temperatures — Not Just Heat Waves — Are Sending a Clear Message

In 1896 a Swedish scientist warned that burning coal would warm the planet. By 1912 Popular Mechanics even celebrated that rising carbon dioxide might bring “milder breezes” to future generations. By the 1970s public sentiment had shifted from optimism to concern, and now the changes forecast more than a century ago are arriving at scales people can feel.
Why Earth Is Not the Moon
When I teach a “Climate Foundations” course at the University of Chicago, I ask students: why isn’t Earth like the Moon? Both bodies receive roughly the same sunlight, yet the Moon swings from blistering daytime heat to frigid nights. Earth’s atmosphere—thin though it is—redistributes heat and contains greenhouse gases (mainly carbon dioxide and water vapor) that trap outgoing infrared radiation. That trapping changes how the planet sheds heat: rather than simply radiating energy to space, Earth loses much of its heat through evaporation and the movement of moist air.
Warming Makes Temperatures More Uniform
Adding more carbon dioxide makes Earth even less moon-like. Temperatures rise overall, but warming is not uniform: colder regions warm faster than warmer ones, nights warm faster than days, and winters warm faster than summers. These are long-term shifts rather than isolated cold snaps or brief heat waves that attract immediate attention. The result can lower some heating bills but it undermines winter recreation and natural ice formation in places that used to reliably freeze.
More Rain — But Also More Dryness
Warmer temperatures increase both evaporation and the atmosphere’s capacity to hold moisture (roughly 6–7% more water per degree Celsius). Climate models typically project global average precipitation to rise on the order of about 1–2% per °C of warming. The combination of faster evaporation and greater moisture capacity means precipitation events tend to be more intense when they occur, but there are often longer dry intervals between storms. That physics explains the apparent paradox of more frequent flash floods alongside drier soils and longer droughts.
Wildfires: Bigger, Hotter, and Farther Afield
Warmer air also dries vegetation more effectively, increasing forest flammability. Longer fire seasons, larger blazes, and fires in regions that historically were less prone to burning are becoming more common. For example, smoke from large fires in central Canada has reached metropolitan areas—Chicago, New York, Washington, D.C.—that once rarely experienced such air quality impacts. Recent summer fires in Western Europe, including large blazes near Bordeaux and in Spain, highlight how heat and drought combine to produce compound risks.
Sea Level Rise and Slow-Onset Changes
Some changes unfold slowly but are effectively locked in by physics. Warmer water expands, so oceans rise even in the absence of additional ice melt. That thermal expansion, together with melting ice, raises long-term risks for coastal communities and infrastructure. Planning for future generations means recognizing that certain places—beachfront lots in low-lying Florida, parts of New Orleans—face growing hazards.
What This Means for Society
These developments are alarming but not inevitable disasters. Earth has experienced higher CO2 and warmer conditions in its distant past, and life persisted. What is different now is the speed of change and the fragility of the human systems that feed and shelter more than eight billion people. Faster, coordinated planning and adaptation—alongside reductions in greenhouse gas emissions—will reduce harm and increase resilience.
Elisabeth Moyer is an Associate Professor in the Department of the Geophysical Sciences at the University of Chicago, a former director of the university’s Center for Robust Decision-making on Climate and Energy Policy, and a faculty affiliate of the Institute for Climate and Sustainable Growth.
Originally published at USA TODAY.
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