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The circulation of the Atlantic Ocean plays a key role in the Global Ocean Conveyor Belt. Credit: Intergovernmental Panel on Climate Change.

The Atlantic Ocean’s circulation is at its weakest in 1,600 years, and this could disrupt weather patterns

The circulation of the Atlantic Ocean plays a key role in the Global Ocean Conveyor Belt. Credit: Intergovernmental Panel on Climate Change.

The circulation of the Atlantic Ocean plays a key role in the Global Ocean Conveyor Belt. Credit: Intergovernmental Panel on Climate Change.

The circulation of the Atlantic Ocean plays a key role in regulating the climate on a global level. Scientists have always known that this constantly moving system of deep-water circulation can vary in amplitude. However, a new study is surprising because it suggests the Atlantic’s circulation is at its weakest point in 1,600 years. If this trend continues, it could disrupt weather patterns all the way from the United States to the African Sahel.

The Little Ice Age and modern global warming

The Atlantic’s deep-water circulation is part of a constantly moving system of deep-ocean circulation driven by temperature and salinity, known as the Global Ocean Conveyor Belt. This system carries warm and salty water from the Gulf Stream to the North Atlantic, warming Western Europe in the process. At the same time, the colder water sinks to a great depth, traveling all the way to Antarctica, ultimately circulating back up the Gulf Stream.

Researchers at the University College London investigated ocean-based sediment records and found that the Atlantic’s overturning began to weaken near the end of the Little Ice Age, a cold period that lasted until 1850. It’s possible to know this by studying the size of sediment grains deposited in time by deep-sea currents — the larger the grains, the stronger the current.

According to Dr. David Thornalley, the study’s lead author, towards the end of the Little Ice Age, freshwater disrupted the Atlantic Meridional Overturning Circulation (AMOC) system. As a result, the warm water started melting Arctic sea ice, ice sheets, and glaciers surrounding the Arctic. This provided a huge influx of freshwater into the North Atlantic, making the surface seawater lighter by diluting it, and consequently slowing down the AMOC system.

Using a combination of methods, the results “suggest that the AMOC has weakened over the past 150 years by approximately 15 to 20 percent” said Thornalley.

Given that North Atlantic circulation is much more variable than previously thought, it’s now important for researchers to incorporate the new findings into climate models. It will also prove interesting to learn why previous models have underestimated AMOC decreases so far.

Elsewhere, another study published in the same issue of the journal Nature, by researchers at the Potsdam Institute for Climate Impact Research, Germany, found that AMOC has been rapidly weakening since the 1950s — and climate change seems to be the main culprit. Together, the studies suggest that AMOC is exceptionally weak today.

“What is common to the two periods of AMOC weakening – the end of the Little Ice Age and recent decades – is that they were both times of warming and melting,” said Thornalley. “Warming and melting are predicted to continue in the future due to continued carbon dioxide emissions.”

Deep Sea Discoveries

dumbo octopusLife emerged and evolved initially in the water – every creature we see today stems from creatures who initially evolved underwater. But even after so much time, there there are many things don’t understand about marine ecosystems, and to be quite honest, the ecosystems we probably know least about are underwater.

Researchers from Fisheries and Oceans Canada and Memorial University of Newfoundland joined their forces and they made a survey of unexplored depths of the Atlantic Ocean for three weeks; they surveyed deep water animal life off the coasts of Nova Scotia and Newfoundland using an underwater robot known as ROPOS (Remotely Operated Platform for Ocean Science) and their focus represented by the corals. The results were weird in a good way. The life in these waters is more diverse than they believed.

They made over 3,000 high quality photographs that displayed this diversity, including an octopus with large fins near its eyes, known as “Dumbo,” a potentially new species of scallop and an organism which was believed not to be found there. This organism is made out of a single cell.

The results were so good that they are going to make another survey next year at the Bedford Institute of Oceanography in Dartmouth. The focus of that is going to be how the newly discovered species fit in the food chain and how they affect it. Findings are very important for biology and medicine, possibly providing valuable medicines.