Summary:
The ocean’s swirling currents, known as eddies, are more intricately connected to atmospheric winds than previously thought.
A new study published in Nature Communications reveals that rather than simply slowing eddies down, atmospheric winds can either dampen or energize them depending on their spin direction. Researchers from the University of Rochester analyzed satellite imagery and high-resolution climate models to uncover this asymmetry, challenging long-held assumptions.
First author Shikhar Rai and senior scientist Hussein Aluie explain that prevailing winds, such as trade winds and westerlies, interact with ocean currents in complex ways, affecting not just eddies but also strain patterns — subtle ocean movements that account for half of the ocean’s kinetic energy.
These findings could improve climate models, enhance ocean observation systems, and offer practical benefits for industries like fisheries and maritime navigation.
How does the atmosphere affect ocean weather?
New research reveals the surprising ways atmospheric winds influence ocean eddies, shaping the ocean’s weather patterns in more complex ways than previously believed.
Much like the windy weather patterns that affect the Earth’s surface, our planet’s oceans experience their own distinct weather patterns. These weather patterns, known as eddies, are circular currents of water that are typically about 100 kilometers wide.
A new study of satellite imagery and high-resolution climate model data by scientists at the University of Rochester upends previous assumptions and provides insight about how those surface and ocean weather patterns interact.
Scientists formerly believed atmospheric wind had a damping effect, slowing the eddies, but the study offers a new theory that better explains the complexities of how atmospheric wind affects eddies.
“It’s actually more interesting than what people had previously thought,” says Hussein Aluie, a professor in the Department of Mechanical Engineering and the Department of Mathematics and senior scientist at the University’s Laboratory for Laser Energetics “There’s a marked asymmetry in how the wind affects these motions, and it depends on the direction they spin.”
Aluie says that prevailing winds that move longitudinally across the globe, such as the westerlies and trade winds, will slow the eddies when they move in the opposite direction but energize them if their spin is aligned.
In between the swirling eddies are intricate tangles of ocean weather patterns known as strain. While strain patterns aren’t as easily distinguished by the naked eye, Aluie says they account for about half of the ocean’s kinetic energy and are damped or energized by wind in similar ways as eddies.
“The new energy pathways between the atmosphere and the ocean that we discovered can help design better ocean observation systems and improve climate models,” says Shikhar Rai ’23 PhD (mechanical engineering), first author of the study and a postdoctoral investigator at Woods Hole Oceanographic Institution. In addition to improving climate modeling, being able to better predict the ocean’s weather patterns could have practical applications for fisheries and help better direct commercial ships where to go.
The study was supported by the National Science Foundation, NASA, the Department of Energy, and the National Oceanic and Atmospheric Administration, focused largely on the mechanical interactions between the atmosphere and the ocean. In future studies, Aluie plans to investigate the role eddies play in transporting energy between the oceans and atmosphere.
Journal Reference:
Rai, S., Farrar, J.T. & Aluie, H., ‘Atmospheric wind energization of ocean weather’, Nature Communications 16, 1172 (2025). DOI: 10.1038/s41467-025-56310-1
Article Source:
Press Release/Material by Luke Auburn | University of Rochester
Featured image credit: NASA | Goddard Space Flight Center Scientific Visualization Studio photo
