Scientists have discovered that the Atlantic Meridional Overturning Circulation (AMOC) is more susceptible to rapid warming than gradual temperature increases, potentially reaching a tipping point at lower temperatures.

The AMOC plays a crucial role in global climate regulation by transporting warm water from the tropics towards the poles and returning cold water back southward.

This new finding suggests that current rates of ocean warming could destabilize this critical circulation system faster than previously estimated, leading to significant climatic impacts.