Atlantic Ocean Current Slowing Raises Concerns for Climate Impact
Recent studies have provided compelling evidence that the Atlantic Meridional Overturning Circulation (AMOC), a crucial component of the global ocean conveyor belt, is weakening. This current transports warm, salty water from the Gulf of Mexico to the North Atlantic, playing a vital role in moderating the climate of Western Europe. Analysis of historical ocean temperature data suggests a 15% reduction in AMOC strength since 1950. Direct measurements, conducted over the past two decades, have now shown a consistent slowing at multiple latitudes in the western Atlantic. The RAPID-MOCHA array, installed by the University of Miami and other institutions, has recorded a decline in AMOC flow by approximately 90,000 cubic meters per second annually since 2004, indicating a 10% weakening by 2023. This trend is attributed to freshwater influx from Greenland's melting ice sheet, which dilutes the dense, salty water, slowing its southward movement.