A paper published in the journal Science Advances is adding to the growing body of research showing that the Atlantic Meridional Overturning Circulation (AMOC) is weakening. In this new study, instead of relying mainly on computer models, scientists used two decades of direct ocean measurements to confirm the decline.
The AMOC is a large system of Atlantic Ocean currents that redistributes heat, salt and nutrients between the tropics and the North Atlantic, helping keep regions like Europe much milder than they would otherwise be. The consequences of a substantial weakening, or indeed a total collapse, could be a potentially catastrophic change in weather conditions.
Taking measurements from the deep
To get a clear picture of what is happening, researchers from the U.S., the UK and Canada looked at data from four sets of underwater sensors called mooring arrays. These are anchored to the sea floor along the western side of the Atlantic, from near the Caribbean up to the waters off Eastern Canada. They measured ocean-bottom pressure and related properties of deep ocean water below 1,000 meters.
By calculating changes in pressure along the continental slope at the western boundary, the team could determine how deep overturning currents were changing over time. Monitoring these changes over time is important because it allows scientists to see a clear, long-term pattern in ocean circulation that might otherwise be hidden by seasonal shifts.
The researchers analyzed over 20 years of data to ensure the decline they observed was a consistent trend rather than a temporary fluctuation.
This decline wasn't in one spot but was observed across all study areas, from 16.5°N (near the Caribbean) to 42.5°N (near Canada). "We identify a meridionally consistent decline in deep western overturning transport across these latitudes over the past two decades," commented the research team in their paper.
An early warning system
The scientists believe this area is the best place to monitor the ocean's health because circulation changes at higher latitudes show up on the western side before they do on the eastern side or in the middle of the Atlantic. Therefore, it could act as an early warning system for the entire Atlantic region. The study authors noted that "This decline, observed at the western boundary, may serve as an effective indicator of AMOC weakening."
Improved monitoring of these currents could help better predict future climate shifts and guide global mitigation strategies.