One Million Years Ago, Our Planet’s Ocean Current Systems Sent Our World into a Deep Freeze

It was something like in the 'The Day After Tomorrow Movie'.

Scientists have revealed that an ocean current system, just like the one that triggered a global Ice Age in the Day After Tomorrow movie, changed the world’s climate around one million years ago.

Around one million years ago, a longtime pattern of alternating glaciations and warm periods dramatically changed, when ice ages suddenly became longer and more intense.

Scientists have long suspected that the slowdown of a key Atlantic Ocean current system influenced the duration of Ice Ages on Earth.

In the 2004 film, ‘The Day After Tomorrow’, our planet’s ocean currents come to a halt as a result of global warming, tossing the entire planet into a catastrophic mini-ice age. Image Credit: Twentieth Century Fox.

A new study of sediments from the Atlantic Ocean’s seabed links the slowdown of the Atlantic Ocean current to the massive buildup of carbon dragged in from the air.

The current, known as the Atlantic meridional overturning circulation (AMOC) is of great importance to our planet and its ocean as it transports warm salty water from near the equator, all the way to northern Europe.

But a number of different processes happen as the current transports water.

The colder water originating from the Arctic makes it become much denser, causing it to sink to the depths. As it sinks, it drags massive amounts of carbon that have been absorbed from our planet’s atmosphere.

This deep water eventually makes its way back to the south, where much of it ends ur reemerging in the Southern Ocean. Scientists have found that this process then releases greenhouse gas back into the atmosphere.

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The study of the ocean seabed and ocean currents has provided conclusive evidence that the current slowed down dramatically, nearly one million years ago.

Scientists believe this is directly connected with a massive build-up of carbon in the waters deep in the Atlantic and a similar decline of carbon in the Earth’s atmosphere.

This combination of events tossed our planet into a series of Ice Ages that started taking place every 100,000 years, instead of the usual 40,000-year-periods.

Scientists refer to this turning point as the Mid-Pleistocene Transition, and the new pattern has persisted right through the last ice age, which ended about 15,000 years ago.

However, the exact reason as to why this pattern has remained is a scientific enigma. The study clearly shows that the carbon missing from the atmosphere ends up in the ocean, and that affects our planet’s climate drastically.

“It’s a one-to-one relationship. It was like flipping a switch,” said lead author Jesse Farmer, who did the work while a Ph.D. student at Lamont-Doherty.

“It shows us that there’s an intimate relationship between the amount of carbon stored in the ocean, and what the climate is doing.”

The study is published in the journal Nature Geoscience.