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Rochester researchers go ÌÇÐÄ´«Ã½˜outside the boxÌÇÐÄ´«Ã½™ to delineate major ocean currents

This illustration by Benjamin Storer shows oceanic currents from satellite data overlaid with large scale circulation currents (gold lines) which can be extracted with a coarse graining technique developed in the lab of Hussein Aluie. Note the most energetic of these currentsÌÇÐÄ´«Ã½” the Antarctic Circumpolar CurrentÌÇÐÄ´«Ã½”at lower left.

Coarse graining technique enables them to ÌÇÐÄ´«Ã½˜gain more by settling for less.ÌÇÐÄ´«Ã½™

For the first time researchers have quantified the energy of ocean currents larger than 1,000 kilometers. In the process, they and their collaborators have discovered that the most energetic is the Antarctic Circumpolar Current, some 9,000 kilometers in diameter.

The team, led by , associate professor of mechanical engineering, used the same coarse-graining technique developed by his lab to previously document energy transfer at the other end of the scale, during the ÌÇÐÄ´«Ã½œeddy-killingÌÇÐÄ´«Ã½� that occurs when wind interacts with temporary, circular currents of water less than 260 kilometers in size.

These new results, reported in , show how the coarse-graining technique can provide a new window for understanding oceanic circulation in all its multiscale complexity, says lead author Benjamin Storer, a research associate in AluieÌÇÐÄ´«Ã½™s . This gives researchers an opportunity to better understand how ocean currents function as a key moderator of the EarthÌÇÐÄ´«Ã½™s climate system.

The team also includes researchers from the University of Rome Tor Vergata, University of Liverpool, and Princeton University.

Traditionally, researchers interested in climate and oceanography have picked boxes in the ocean 500 to 1,000 square km in size. These box regions, which were assumed to represent the global ocean, were then analyzed using a technique called Fourier analysis, Aluie says.

ÌÇÐÄ´«Ã½œThe problem is, when you pick a box, you are already limiting yourself to analyzing whatÌÇÐÄ´«Ã½™s in that box,ÌÇÐÄ´«Ã½� Aluie says. ÌÇÐÄ´«Ã½œYou miss everything at a larger scale.

ÌÇÐÄ´«Ã½œWhat we are saying is, we donÌÇÐÄ´«Ã½™t need a box; we can think outside the box.ÌÇÐÄ´«Ã½�

When the researchers use the coarse-graining technique to ÌÇÐÄ´«Ã½œblurÌÇÐÄ´«Ã½� satellite images of global circulation patterns, for example, they find that ÌÇÐÄ´«Ã½œwe gain more by settling for less,ÌÇÐÄ´«Ã½� Aluie says. ÌÇÐÄ´«Ã½œIt allows us to disentangle different-sized structures of ocean currents in a systematic way.ÌÇÐÄ´«Ã½�

He draws an analogy to removing your eyeglasses, then looking at a very crisp, detailed image. It will appear to be blurred. But as you look through a succession of increasing stronger eyeglasses, you will often be able to detect various patterns at each step that would otherwise be hidden in the details.

In essence, that is what coarse graining allows the researchers to do: quantify various structures in ocean current and their energy ÌÇÐÄ´«Ã½œfrom the smallest, finest scales to the largest,ÌÇÐÄ´«Ã½� Aluie says.

Aluie credits Storer for further developing and refining the code; it has been published so other researchers can use it.

Other collaborators include Michele Buzzicotti, a research scientist at the University of Rome Tor Vergata; Hemant Khatri, a research associate at the University of Liverpool, and Stephen Griffies, a senior scientist at Princeton.

Support for the project included funding from the National Science Foundation, the National Aeronautics and Space Administration, and the Department of Energy.


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