Recent scientific findings highlight the weakening of the Atlantic Meridional Overturning Circulation (AMOC), a crucial ocean current system affecting global climate. The AMOC, often called the 'Atlantic conveyor belt,' transports warm, salty water from the tropics northward, moderating Europe's climate. New research, based on buoy measurements, reveals a concerning 10% reduction in AMOC's flow between 2004 and 2023, amounting to a decline of approximately 90,000 cubic meters of water per second each year. This weakening is primarily attributed to the influx of freshwater from the melting Greenland ice sheet, which dilutes the ocean's salinity and disrupts the sinking process essential for the AMOC's function.