Why the Planet Paused Its Warming

Original: "Anthropogenic contributions to slow warming over 1998-2012"
arXiv:2309.13862 · 2023-09-25 · CC BY 4.0 · 1 min
From 1998 to 2012, Earth warmed more slowly, and scientists figured out what helped cool it: a cold ocean, a quiet Sun, and our own efforts.

Earth's climate is like an orchestra where each instrument plays at its own tempo. The ocean, the Sun, volcanoes, and human activity pull temperature in different directions. From 1998 to 2012, that orchestra seemed to slow down: the planet warmed more slowly than before, even though greenhouse gas emissions were breaking records. Scientists long debated why.

It turned out that the main brakes were two natural factors: the cool La Niña current in the Pacific Ocean and a period when the Sun shone a bit less brightly. Together they explained about three-quarters of the slowdown.

But a quarter remained, and that was explained by people themselves. We have been emitting less methane and ozone-depleting substances, gases that strongly warm the atmosphere. This happened thanks to international agreements, such as the Montreal Protocol. Scientists calculated that this reduction in emissions slowed warming by about 24%. That is good news: it means our efforts to clean the air are already working, and we can influence the climate faster than we thought.

The 1998-2012 warming slowdown was sometimes called a 'pause' in global warming, but more recent data with gap-filling in the Arctic showed that the pause was not as deep as previously thought.

In Kim Stanley Robinson's novel 'The Ministry for the Future', humanity's attempts to manage the climate are described, including reducing methane emissions. This study shows that such measures can indeed have a measurable effect in real time.

DDT = trend_{1998-2012} - trend_{1951-2012}
A measure of warming slowdown or acceleration: a negative value indicates slowdown
Concepts
global warming La Niña greenhouse effect El Niño seasonal forcing annual cycle climate troposphere North Atlantic Oscillation UAH satellite record land carbon sink El Niño-Southern Oscillation ocean-atmosphere coupling relative ONI carbon cycle ENSO climate model sea surface temperature anomaly atmospheric pressure Indian Ocean capacitor effect