Amoc, the Atlantic meridional overturning circulation, is a vast movement of water deep in the Atlantic. It carries warm water from the tropics towards Greenland, where it cools and sinks before returning south at depth. Recent studies suggest that this circulation is weakening. If it slows more, northern Europe could see much colder winters even as the planet warms. Tropical monsoons could shift, and sea levels could suddenly rise along the US east coast. Yet Amoc rarely stays in the news for long. One reason is that it is difficult to picture. Journalists often rely on maps, arrows, or other simple images, because the current itself is mostly hidden below the surface.
Why this Atlantic current is hard to show
Amoc is a huge flow of water in the Atlantic that carries heat north. Studies suggest that it is weakening. If it slows further, the effects could include colder winters in northern Europe, changes in tropical monsoons, and sudden sea level rise on the US east coast.

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