Page 7: 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.

Tiny turbulent whirls keep the Arctic ocean flowing

In the coming decades, climate change is likely to lead to a loss of sea ice in and an influx of warmer water to the Arctic Ocean, affecting the ocean's vertical circulation. Brown and colleagues recently investigated the ...

How to make AMOC model experiments more realistic

Melting ice in the Arctic is causing an increasing amount of freshwater to enter the North Atlantic, which is expected to result in a weakening of the Atlantic overturning circulation. However, many modeling studies make ...

Regional ocean dynamics can be better emulated with AI models

The Gulf of Mexico, a regional ocean, is hugged by the southeastern United States and a large stretch of the Mexican coast, making it very important for both countries. The area helps bring goods to local and global markets, ...

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