China’s significant reductions in air pollution may have brought unexpected benefits to the Arctic. A new study shows that aerosol-driven storms have decreased, resulting in less sea ice loss. But at the same time, experts say this drastic drop in aerosols may have accelerated global warming.
“The Chinese people have been suffering from poor air quality for decades,” Bjorn Samsett, a senior researcher at the CICERO International Climate Research Center in Norway, told Live Science. “This pollution temporarily slowed global warming, and the rest of the population took a little longer to adapt to a warmer climate. What is happening now is that we are seeing the full effects of warming due to greenhouse gases, and in any case, we will have to face it sooner or later.”
In late January 2019, wind patterns in the North Pacific changed, causing five powerful cyclones to slam into the Bering Sea in quick succession. Each blew warm southerly winds onto the ice, breaking it up and pushing it north. Temperatures in the northern Bering Sea were 21.6 to 28.8 degrees Fahrenheit (12 to 16 degrees Celsius) above normal. By early March, ice area had decreased by 82%. This represents a retreat of approximately 154,440 square miles (400,000 square kilometers), the largest decline recorded by satellite during this period.
you may like
Scientists have long known that cyclones can destroy sea ice in the Arctic. What they’re less sure about is what sends the storm there in the first place.
The new study, published March 18 in the journal NPJ Climate and Atmospheric Science, provides an unexpected answer. From 2000 to 2014, smog rising from China’s smokestacks may have steered winter storms north into the North Pacific Ocean, sending more storms into the Arctic and destroying ice in the Bering Sea.
To understand how soot and sulfate particles in the skies over the Pacific Ocean affect ice off the coast of Alaska, it helps to think about what happens during storms. Mid-latitude cyclones, the comma-shaped swirling systems that produce much of the Northern Hemisphere’s winter weather, all operate on a type of heat engine. Warm, moist air evaporates near the ocean surface and rises to form clouds, releasing heat that fuels storm circulation.
Aerosols (the tiny particles that make up industrial haze) disrupt this engine in subtle but significant ways. Water vapor typically condenses around a relatively small number of particles, forming large droplets that quickly fall as rain on the south side of the storm. But if the air is filled with aerosols, each particle seeds a cloud droplet. The result is a large number of small droplets that do not immediately become raindrops. Precipitation on the southern flank of the storm is suppressed and moisture moves further along the storm’s conveyor belt toward the northeastern flank, where it releases heat. This is exactly the right place to push the entire system towards the poles.
Lead author Dianbin Cao, a researcher at the Institute of Tibetan Plateau Research at the Chinese Academy of Sciences, and his colleagues combined 40 years of observational data and climate model simulations to examine how aerosol levels in East Asia affected the path of winter cyclones across the North Pacific. The researchers compared the 14 years of elevated aerosol loads from 2000 to 2014 with the 15 years of lower aerosol levels in previous decades, and found that cyclone tracks moved north by up to 1.23 degrees by the time the storms subsided. This is enough to nearly double the number of cyclones entering the Arctic.
Alex Crawford, an Arctic climate scientist at the University of Manitoba who studies the interaction between cyclones and sea ice but was not involved in the study, said the pressure on storm systems from this aerosol is “stronger than I thought.” “They did a very good job of demonstrating the mechanisms by which aerosols influence extratropical cyclones.”
When these storms reach the Bering Sea, the effects can be dramatic. The cyclone’s counterclockwise winds push the ice back toward the Chukchi Sea between Alaska and Russia. Waves break the ice floes. Strong winds from the south bring warm air and temperatures can reach sub-zero temperatures even in the middle of winter, as happened very severely in 2019.
What to read next
However, there are possible signs of hope. China’s air pollution cleanup, which began in 2013, has proven to be one of the most effective environmental interventions in history, reducing the country’s sulfate aerosol emissions by about 75% in about 10 years. The study suggests that this reduction “could potentially mitigate the poleward shift in storm tracks caused by global warming,” sparing the Arctic some of the damage caused by extratropical cyclones.
But the picture is more complex. Aerosols also cool the Earth by reflecting solar radiation back into space and brightening clouds. When they disappear, their cooling effect is also gone, thereby revealing greenhouse gas warming that has been suppressed for decades. A 2025 study led by Samset, which was not involved in the new study, found that a decline in aerosols in East Asia is significantly accelerating global warming.
The reduction in aerosols, which could alleviate cyclone pressure on the Bering Sea, is also revealing the full effects of global warming.
What this climate tug-of-war means for Arctic sea ice remains to be seen, but Dan Westervelt, an atmospheric scientist at Columbia University’s Lamont-Doherty Earth Observatory and co-author of the Samsett 2025 study, thinks warming effects will prevail. “Warming is more permanent and can occur in all seasons, so unmasked warming will probably dominate, whereas changes in storm tracks will probably be more temporary,” he told Live Science.
Westervelt said the study shows that aerosols have a larger and more complex influence on Earth’s climate than previously realized. “The speed of aerosol reduction in East Asia has been underestimated,” he said. “What took 30 years to reduce emissions in North America and Europe took 10 years in East Asia. How this affects cyclones and Arctic warming will be very interesting to study and is critical for climate mitigation and adaptation.”
Cao, D., Xu, D., Lin, Y., Deng, Y., Chen, X., Zhang, Q., Gao, M., and Zhang, X. (2026). Anthropogenic aerosols can shape the paths of winter midlatitude cyclones. Npj climate and atmospheric science. https://doi.org/10.1038/s41612-026-01377-w
Source link
