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Scientists at MIT have now identified a key mechanism, which they call the "ice-ocean governor," that controls how fast the Beaufort Gyre spins and how much fresh water it stores. In a paper published today in Geophysical Research Letters, the researchers report that the Arctic's ice cover essentially sets a speed limit on the gyre's spin.
In the past two decades, as temperatures have risen globally, the Arctic's summer ice has progressively shrunk in size. The team has observed that, with less ice available to control the Beaufort Gyre's spin, the current has sped up in recent years, gathering up more sea ice and expanding in both volume and depth.
Temperatures - Researchers - Mechanism - Gyre - Spin
If global temperatures continue to climb, the researchers expect that the mechanism governing the gyre's spin will diminish. With no governor to limit its speed, the researchers say the gyre will likely transition into "a new regime" and eventually spill over, like an overflowing bathtub, releasing huge volumes of cold, fresh water into the North Atlantic, which could affect the global climate and ocean circulation.
"This changing ice cover in the Arctic is changing the system which is driving the Beaufort Gyre, and changing its stability and intensity," says Gianluca Meneghello, a research scientist in MIT's Department of Earth, Atmospheric and Planetary Sciences. "If all this fresh water is released, it will affect the circulation of the Atlantic."
Meneghello - Co-author - Paper - John - Marshall
Meneghello is a co-author of the paper, along with John Marshall, the Cecil and Ida Green Professor of Oceanography, Jean-Michel Campin and Edward Doddridge of MIT, and Mary-Louise Timmermans of Yale University.
A "new Arctic ocean"
Handful - Times - Past - Beaufort - Gyre
There have been a handful of times in the recorded past when the Beaufort Gyre has spilled over, beginning with the Great Salinity Anomaly in the late 1960s, when the gyre sent a surge of cold, fresh water southward. Fresh water has...
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