Page 9: Research news on ocean circulation

Ocean circulation refers to the large-scale, coherent movement of seawater driven primarily by wind stress, density gradients (thermohaline processes), Earth’s rotation, and basin geometry. It encompasses wind-driven gyres, western boundary currents, and the global overturning circulation that links surface and deep waters across ocean basins. Ocean circulation redistributes heat, salt, carbon, nutrients, and tracers, thereby regulating climate, biogeochemical cycles, and sea level. It is studied using in situ observations, satellite remote sensing, numerical models, and theory, with key research focusing on circulation variability, its sensitivity to forcing (e.g., greenhouse gas–induced warming and freshwater input), and associated feedbacks in the climate system.

Shaped by paleogeography: A new world map of marine mollusks

Biogeographical regions of marine organisms, i.e., their distribution across different habitats, often overlap well with the major global ocean currents. The geological age of the currents plays a major role in this. The ...

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 ...

Water density shifts can drive rapid changes in AMOC strength

In the Atlantic Ocean, a system of currents carries vast amounts of warm, salty surface water northward. As this water reaches higher latitudes and becomes colder, it sinks and joins a deep, southward return flow. This cycle, ...

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