Heatwaves can reverse decades of air pollution progress
 
 

China has spent more than a decade cleaning up its air. Regulations cut pollution from cars, factories, and power plants, leading to dramatic improvements across much of the country.

Fine particle pollution dropped, season after season. Then the summer of 2022 arrived when ozone climbed instead of falling. The heat seemed to turn against the cleanup.

A team at Fudan University set out to investigate, in collaboration with researchers at Duke University and the University of California, Irvine (UCI).

Heat boosted ozone pollution

Heat works on plants and soil alike. When it climbs, trees and shrubs pump out more terpenoids – a family of reactive carbon compounds.

The soil contributes too. It breathes out more nitrogen oxides at the very same time.

Scientists had clocked each response on its own for years. Nobody had watched the two surge at once.

Their chemistry would collide in the same hot air. That blind spot matters more now than before.

Human-made pollution keeps falling each year. The natural sources fill the space it leaves behind.

When the heat hit

The summer of 2022 shattered records nationwide. Average temperatures climbed from about 73 to 77 degrees Fahrenheit. One reading hit a brutal 115 degrees.

The Yangtze River Basin caught the worst of it. During the hottest spells, some areas there ran about 11 degrees Fahrenheit above normal.

As the heat built, the soil dried out. Some patches of the basin shed more than half their moisture.

The drought only bit harder after that. Ozone shadowed the heat almost step for step. Basin-wide, the daily ozone measure jumped 21 percent over the 2020 to 2021 average.

That spike dwarfs the slow creep of earlier years. From 2013 to 2019, ground readings had inched up about 1.9 ppb a year.

Trees that prime the air

The heat sent terpenoid emissions soaring. Isoprene leads that group of compounds.

In the hardest-hit areas, it shot up more than 130 percent above the old average.

Satellite readings of formaldehyde told the same story. They rose about 31 percent over the basin, close to the model’s own figure.

Those extra terpenoids did more than add fuel. They cranked up the air’s power to oxidize other chemicals, a trait researchers call oxidation capacity.

How ozone pollution formed

Here is the mechanism the team uncovered. As terpenoids break down, they spin off reactive fragments called peroxy radicals.

Those radicals grab nitric oxide straight from the soil. They turn it into nitrogen dioxide. Normally that switch eats up ozone. This pathway skips the step.

Sunlight then splits the nitrogen dioxide back apart. Fresh ozone forms in its place. So the soil nitrogen drives ozone upward. The usual brake never gets applied.

A clue sat buried in the data. Human-made nitrogen oxides have been falling under China’s Clean Air Action Plan, yet nitrogen dioxide over the basin still rose through the heat.

The soil, not the traffic, was the likely culprit. That one mismatch tied the extra ozone back to the ground.

The toll on one basin

The combined effect bit hardest where nitrogen, not carbon, caps ozone formation. That covers much of the Yangtze River Basin.

Secondary organic aerosol rose right alongside the ozone. This fine particle forms straight from terpenoids.

In the worst spots it climbed by up to four micrograms per cubic meter. Both halves of the pollution problem worsened at once.

Heat thresholds increased pollution

The temperature thresholds stood out in the record.

Aerosol jumped about 50 percent past 86 degrees Fahrenheit, while the sharpest ozone rise held off until past 95.

The regional picture held a cruel twist.

Fine particles kept falling across most of China that summer, yet a few cities in the Sichuan and Chongqing area watched both ozone and particles climb.

Nature increased ozone pollution

The authors said the strength of the natural feedback loop came as a genuine surprise.

They noted that, while reductions in human-caused emissions had long been viewed as a success, nature appeared to be pushing back in unexpected ways.

“The vegetation and the soil are essentially conspiring during heatwaves – the trees pump out these reactive compounds that supercharge the atmosphere’s oxidation capacity, which then grabs the nitrogen coming out of the soil and turns it into ozone much faster than we thought possible,” the researchers noted.

“If we don’t account for this in our pollution control strategies, we could be chasing our tails as the climate continues to warm.”

Why progress can stall

China keeps trimming its human-made nitrogen oxides. With each cut, more of the country slides into the chemical state where this loop bites hardest.

Those nitrogen-limited zones keep spreading outward. The cleaner the cities get, the more room the loop has to work.

Further cuts may pay off less than planners expect on hot days. The authors call their numbers a floor, not a ceiling.

The model probably undercounts soil nitrogen. So the real effect may run stronger than the figures suggest.

Planting trees, with care

The findings raise an awkward point about greening. Big tree-planting drives lock away carbon, which the climate badly needs.

But more trees also mean more terpenoids. Planted with no regard for local chemistry, large forests could foul the very air around them.

The authors want forest planning to weigh atmospheric chemistry too. Done right, greening and clean air can pull in the same direction.

Warming worsens ozone pollution

The team also ran a warmer world. Pushing temperatures up by about nine degrees Fahrenheit, in line with a high-emissions path, almost doubled the effect.

That hints at summers where heatwaves bring more than discomfort. They could bring dirtier air the cleanup never planned for.

The researchers urge policymakers to fold shifting natural emissions into their plans. Pollution control aimed only at human sources may keep losing ground as the planet warms.

The study is published in the journal Environmental Science and Ecotechnology.

NOTE – This article was originally published in Earth and can be viewed here

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