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A new study finds that recent changes in air pollution are not the main reason the growing \u201cenergy imbalance\u201d that is fueling global warming has increased.<\/p>\n
Aerosols\u2014tiny airborne particles from sources such as pollution, wildfires, and volcanoes\u2014can affect how clouds form and how much sunlight Earth reflects back to space. While aerosols can influence climate regionally, the new research shows their recent global impact has been small.<\/p>\n
The study analyzed nearly two decades of satellite observations combined with modern atmospheric reanalysis data. The researchers found that aerosol changes have affected the climate in opposite ways in the two hemispheres.<\/p>\n
In the Northern Hemisphere, cleaner air in heavily industrialized regions has reduced the number of particles that help clouds reflect sunlight, allowing more solar energy to reach Earth\u2019s surface. In contrast, the Southern Hemisphere has seen large increases in natural aerosols from events such as the 2019\u20132020 Australian wildfires and the 2022 Hunga Tonga\u2013Hunga Ha\u2019apai volcanic eruption. These particles made clouds brighter and more reflective, sending more sunlight back to space.<\/p>\n
Together, the opposing effects largely cancel each other out, resulting in little net global influence from aerosols on Earth\u2019s rising heat imbalance.<\/p>\n
The study also shows that the recent increase in Earth\u2019s energy imbalance is driven mainly by changes in reflected sunlight, rather than by changes in heat escaping to space. From 2003 to 2023, Earth gained heat at a rate of about half a watt more energy per square meter each decade, largely because the planet is absorbing more sunlight.<\/p>\n
To track how aerosols are changing over time, the researchers used two independent indicators. One came from satellites that observe how aerosols in the air affect the passage of sunlight through the atmosphere. The other came from reanalysis data, which combine observations and models to estimate sulfate particles produced by pollution, volcanoes, and wildfires. Despite their different approaches, both methods revealed the same pattern\u2014declining aerosols in the Northern Hemisphere and increasing aerosols in the Southern Hemisphere\u2014indicating that aerosols have had little overall effect on the global energy trend.<\/p>\n
\u201cUnderstanding this hemispheric \u2018balancing act\u2019 helps society focus on the true forces behind global warming\u2014changes in cloud behavior linked to surface warming and natural climate variability\u2014rather than mistakenly attributing recent warming to cleaner air,\u201d says Chanyoung Park, lead author of the study and a doctoral student in the atmospheric sciences department f at the Rosenstiel School.<\/p>\n
\u201cEven though the Northern Hemisphere may experience some regional warming due to reduced aerosols, this does not translate to a significant global impact. This clarity supports better climate planning, more accurate public communication, and informed policy decisions.\u201d<\/p>\n
The findings also highlight a potential limitation in some climate modeling studies, which focus mainly on pollution reductions in the Northern Hemisphere and may underestimate the growing influence of natural aerosol events in the Southern Hemisphere.<\/p>\n
\u201cEarth\u2019s energy imbalance tells us how fast heat is building up in the climate system,\u201d says Brian Soden, a coauthor of the study and a professor in the atmospheric sciences department at the Rosenstiel School.<\/p>\n
\u201cMany earlier studies suggested that cleaner air might explain much of the recent increase, but our results show that aerosol changes largely cancel out between the Northern and Southern Hemispheres. That means we need to look more closely at changes in clouds and natural climate variability to understand why the planet is continuing to gain heat.\u201d<\/p>\n