Page 2: Research news on ocean conveyor belt

The ocean conveyor belt, scientifically termed the global meridional overturning circulation (MOC), is a planetary-scale, density-driven circulation system that links surface and deep waters across all major ocean basins. It is governed primarily by thermohaline processes, whereby variations in temperature and salinity control seawater density, inducing deep-water formation in high-latitude regions (e.g., North Atlantic) and upwelling in lower latitudes and the Southern Ocean. This circulation redistributes heat, dissolved gases, nutrients, and biogeochemical tracers, exerting strong control on Earth’s climate system, carbon cycle, and deep-ocean ventilation on decadal to millennial timescales.

New gravity mission will detect weakening ocean conveyor

At this year's Living Planet Symposium, attendees heard how ESA's Next Generation Gravity Mission could provide the first opportunity to directly track a vital ocean circulation system that warms our planet—but is now weakening, ...

How Greenland's glacial troughs influence ocean circulation

The Atlantic Meridional Overturning Circulation (AMOC) serves as the Atlantic Ocean's conveyor belt, transporting warm water north toward the Arctic Circle and returning cold, dense water back to the tropics. Nearshore areas ...

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