Atlantic Meridional Overturning Circulation

🧬 AI profile — grown from 6ic coverage The Atlantic Meridional Overturning Circulation (AMOC) is a critical component of the global ocean circulation system, responsible for transporting warm water from the equator towards the North Pole and cold water from the North Pole towards the equator. This thermohaline circulation plays a crucial role in regulating Earth's climate by distributing heat around the globe, with a weakening AMOC potentially leading to increased sea levels and altered regional climates. AMOC's health is closely linked to the melting of icebergs and glaciers, which can disrupt the circulation's delicate balance.