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June 17, 2025

Human-caused stratospheric cooling may have been detectable as early as 1885

Model fingerprints of atmospheric temperature change in response to combined anthropogenic and natural external forcing. Credit: Proceedings of the National Academy of Sciences (2025). DOI: 10.1073/pnas.2500829122
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Model fingerprints of atmospheric temperature change in response to combined anthropogenic and natural external forcing. Credit: Proceedings of the National Academy of Sciences (2025). DOI: 10.1073/pnas.2500829122

A small, multi-institutional team of climate scientists has found evidence that human-caused impacts on the stratosphere began earlier than previously thought. In their study, in the Proceedings of the National Academy of Sciences, the group used observational data, environmental theory and computer modeling to create simulations depicting the state of the stratosphere to a time just after the dawn of the industrial age.

Sometime during the 1850s, scientists discovered that carbon could trap heat—but it took another century for scientists to agree that rising CO2 in the atmosphere was causing global warming. Such findings came about due to improvements in technology, such as satellites, weather balloons and ground-based monitoring stations around the globe.

The team first posed a simple question: How far back in time could changes to the stratosphere due to human activities be observed if modern tools had been available?

To find out, they embarked on a study of the stratosphere—the part of the atmosphere above the troposphere. As warm the planet, the stratosphere grows cooler. This cooling is less impacted by changing weather patterns and is thus a more reliable means of detecting changes wrought by human activities.

In modern times, temperatures in the stratosphere can be taken using satellite data. To predict changes in stratospheric temperature before modern tools arrived, the research team used historical data, theory and nine to predict the impact of human-based emissions on temperatures in the stratosphere going back to 1860—the beginning of the industrial age. They found that evidence of changes to the stratosphere due to human activities would have been detectable as far back as 1885.

This was prior to the introduction of automobiles. But humans have been releasing carbon into the atmosphere in other ways for thousands of years through burning coal, wood and other materials, for heating, cooking and manufacturing.

More information: Benjamin D. Santer et al, Human influence on climate detectable in the late 19th century, Proceedings of the National Academy of Sciences (2025).

Journal information: Proceedings of the National Academy of Sciences

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Simulations combining historical data, environmental theory, and climate models indicate that human-induced stratospheric cooling could have been detectable as early as 1885. This cooling, linked to increased greenhouse gas emissions since the industrial age, predates widespread automobile use and reflects earlier human activities such as coal and wood burning.

This summary was automatically generated using LLM.