🌊The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the global Thermohaline Circulation or Global Ocean Conveyor Belt.
⚠️The AMOC is at risk of slowing down due to increased levels of atmospheric CO2, accelerated melting of the Greenland ice sheet, and decreasing sea ice volume in the Arctic.
🌡️A slowdown in the AMOC could lead to a cooling effect in the North Atlantic region and increased storminess across Europe, as well as worsening droughts and sea-level rise in other parts of the world.
📉Research suggests that the AMOC has reached its lowest point since records began in 1880, and models project a further weakening in the future.
💡Scientists are working on developing early warning monitoring systems to track medium-term variations in salinity levels and predict an AMOC collapse decades in advance.