Scientists explain how carbon dioxide cools the stratosphere

Researchers at Columbia University have identified the precise mechanism by which rising carbon dioxide levels cool the upper atmosphere. The finding accounts for decades of observed stratospheric cooling amid surface warming. Their study appears in the journal Nature Geoscience.

The stratosphere, the layer between roughly 11 and 50 kilometers above the surface, has cooled by about 2 degrees Celsius since the mid-1980s. This cooling exceeds by more than ten times the amount expected without human emissions of carbon dioxide. The process was first predicted in the 1960s by climatologist Syukuro Manabe.

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Scientists analyzing ancient ice from Antarctica have found that ocean temperatures dropped by 2 to 2.5 degrees Celsius over the past 3 million years, while carbon dioxide and methane levels changed only modestly. The studies, led by researchers from Oregon State University and others, suggest factors beyond greenhouse gases drove much of Earth's long-term cooling. The findings come from ice cores at Allan Hills in East Antarctica.

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Emissions of carbon monoxide and volatile organic compounds have contributed significantly to planetary warming, according to new research. These indirect greenhouse gases account for about 15 percent of the temperature rise since pre-industrial times. Few nations currently address them in climate plans.

A major Atlantic Ocean current system that regulates global climate has been slowing down for nearly 20 years. New research provides direct evidence of the decline across a wide area of the North Atlantic.

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Researchers have demonstrated in laboratory experiments that hydrogen can be produced from iron-rich rocks while simultaneously locking away carbon dioxide. The work, presented at a recent geoscience meeting, aims to combine clean energy generation with climate mitigation. Field trials are now being planned to test the approach at scale.

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