At the heart of this system lies one of the great mysteries of modern oceanography: the global “thermohaline circulation,” also known as the Atlantic Meridional Overturning Circulation, or AMOC. Scientists are still trying to understand just how stable it is.

A System Powered by Salt, Heat, and the Planet's Rotation

The word thermohaline comes from thermo (heat) and haline (salt). Together, they explain how this immense conveyor belt works. Warm, salty water flows north from the tropics into the North Atlantic (above) where it cools, becomes denser, and sinks deep into the ocean. This deep water then flows south again and eventually resurfaces in distant oceans, completing a global loop.

This movement is not driven only by temperature and salt. Earth’s rotation—the spinning of the planet—helps keep the oceans moving, shaping major currents through what is called the Coriolis effect. If our planet did not rotate, surface currents like the Gulf Stream and deep water pathways would behave in dramatically different ways. In short, Earth's rotation gives the oceans their swirling, looping, planet-wide choreography.

The Climate Connection

Why does all this matter?

Because this global circulation system carries huge amounts of heat. For example, the warm water transported northward is one reason Western Europe has relatively mild winters—compared to places at the same latitude in Canada. If the AMOC were to cease, the distribution of heat around the planet would change, fast!

Could the AMOC Collapse?

Here’s where the mystery deepens. As Arctic ice melts, it releases large amounts of freshwater into the North Atlantic. Freshwater is less dense than salty water, which means it interferes with the “sinking” part of the cycle that drives the AMOC. Some climate models have raised a troubling possibility: If enough freshwater floods the region, the AMOC could weaken—or even collapse.

A collapse would not look like a Hollywood disaster wave. It would be slower, but the consequences would be dramatic. There would be colder winters in parts of Europe, shifts in tropical monsoons, changes in marine ecosystems, sea level rise, and altered storm tracks on both sides of the Atlantic.

Not all scientists agree on how likely or how soon such a shift could occur. The AMOC has fluctuated in the past, but today’s rapid Arctic melt makes the situation unprecedented. What we do know is that the system is complex, poorly understood, and crucial to global climate stability.

A Giant System Scientists are Still Trying to Understand

Despite satellites, deep-ocean sensors, and improved climate models, the AMOC remains one of the least predictable pieces of the climate puzzle. It may be more stable than we think—or more fragile. Though there is little doubt that it will slow as global warming increases, whether there will be an abrupt change before the end of the century is uncertain.

For divers, this makes the ocean feel even more mysterious. Beneath the surface, currents are not just local swirls or tidal surges; they’re part of a worldwide network that helps keep our climate in balance. The more we learn, the more we realise how extraordinary—and how delicate—these underwater highways really are.

(c) Ila France Porcher

Ethologist Ila France Porcher, author of The Shark Sessions and The True Nature of Sharks, conducted a seven-year study of a four-species reef shark community in Tahiti and has also studied sharks in Florida with shark-encounter pioneer Jim Abernethy. Her ethological observations, the first of their kind, have yielded valuable details about the reproductive cycles, social biology, population structure, daily behaviour patterns, roaming tendencies, and cognitive abilities of sharks. Visit: ilafranceporcher.wixsite.com