Recent observations indicate significant changes in the Atlantic Ocean currents, which are vital for regulating global climate patterns. The Atlantic Meridional Overturning Circulation (AMOC), a major component of these currents, is showing signs of weakening, potentially due to increased freshwater input from melting ice and altered precipitation patterns. The AMOC functions as a massive conveyor belt, transporting warm surface water from the tropics towards the North Atlantic, where it cools and sinks, driving circulation and distributing heat across the planet.