Scientists Use Satellites to Help Detect Deep-Ocean Whirlpools

meddes, shown in red, in Atlantic Ocean Coupling data collected by several different satellite-borne sensors, researchers have been able to "break through" the ocean's surface to detect "Meddies" -- super-salty warm-water eddies that originate in the Mediterranean Sea and then sink more than a half-mile underwater in the Atlantic Ocean. The Meddies are shown in red in this scientific figure. Image credit: Univ. of Delaware
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March 20, 2006

Move over, Superman, with your X-ray vision. Marine scientists have figured out a way to see through the ocean's surface and detect what's below, with the help of satellites.

Using sensor data from several U.S. and European satellites, researchers from NASA's Jet Propulsion Laboratory, Pasadena, Calif.; the University of Delaware, Newark; and Ocean University of China, Qingdao; have developed a method to detect salty, submerged eddies called "Meddies" that occur in the Atlantic Ocean off Spain and Portugal at depths of more than 1,000 meters (one-half mile).

These warm, deep-water whirlpools, part of the ocean's complex circulatory system, help drive the ocean currents that moderate Earth's climate. The research marks the first time scientists have detected this phenomenon from space, and the first use of a new multi-sensor technique that can track changes in ocean salinity. Results are reported in the April issue of the American Meteorological Society's Journal of Physical Oceanography.

"Since Meddies play a significant role in carrying salty water from the Mediterranean into the Atlantic, new knowledge about their trajectories, transport and life histories is important to understanding their mixing and interaction with North Atlantic water," said Professor Xiao-Hai Yan of the University of Delaware, lead author of the study and co-director of the university's Center for Remote Sensing. "Ultimately, we hope this will lead to a better understanding of their impact on global ocean circulation and global climate change."

First identified in 1978, Meddies are so named because they flow out of the Mediterranean Sea. A typical Meddy averages about 600 meters (2,000 feet) deep and 100 kilometers (60 miles) in diameter, and contains more than 900 billion kilograms (a billion tons) of salt.

While warm water ordinarily resides at the ocean's surface, the warm water flowing out of the Mediterranean Sea has such a high salt concentration that when it enters the Atlantic Ocean at the Strait of Gibraltar, it sinks to depths of more than 1,000 meters (one-half mile) along the continental shelf. This underwater river then separates into clockwise-flowing Meddies that may continue to spin westward for more than two years, often coalescing with other Meddies to form giant, salty whirlpools that may stretch for hundreds of miles.

"Since the Mediterranean Sea is much saltier than the Atlantic Ocean, the Meddies constantly add salt to the Atlantic," Yan said. Without this steady salt-shaker effect, he notes, the conveyor belt of ocean currents that help distribute heat from the tropics toward the North Pole might be diminished, resulting in colder temperatures in regions such as New England and northwestern Europe that currently experience more temperate climates.

"There is concern about global climate change shutting down the ocean currents that warm the Atlantic Ocean," Yan saids. "The melting of sea ice at the North Pole could add enormous amounts of fresh water to the Atlantic, reducing its salinity enough to slow the sinking of cooler water, which would shut down the conveyor belt of ocean currents that help warm major regions of the planet."

Yan and his team drew on data from several satellite sensors that can read an important signal of a Meddy's presence. Altimeters flying aboard NASA's Topex/Poseidon and Jason satellites and the European Space Agency's European Remote Sensing and Environment (Envisat) satellites measured the height of the sea surface compared to average sea level, revealing the difference in altitude where a Meddy entered the Atlantic.

Specialized microwave radars called scatterometers, including the former NASA Scatterometer (Nscat) on Japan's Midori-1 spacecraft and the current SeaWinds instrument on NASA's QuikScat spacecraft, measured the surface wind over the ocean, providing data needed to remove the surface variability "noise" caused by the wind blowing over the ocean's surface.

"By carefully removing the stronger surface signatures of upper ocean processes, we were able to unveil the surface signatures of deeper ocean processes, such as the Meddies, to these space-based sensors," said Dr. W. Timothy Liu, QuikScat project scientist at JPL.

The scientists also analyzed data provided by an infrared spectrometer known as the Advanced Very High Resolution Radiometer, which flies aboard National Oceanic and Atmospheric Administration satellites. This instrument maps heat emitted by the ocean's top layer and showed the increase in temperature from a warm Meddy before it began sinking.

While the technique is not yet 100 percent accurate, Yan and his colleagues are continuing to refine it, and are exploring its application to other coastal regions of the world. They are currently examining salinity variations in the East China Sea before and after the building of the Three Gorges Dam, the largest dam in the world. The data will help researchers assess the dam's impacts on the ecosystem and on water circulation patterns.

For more information, visit:

http://sealevel.jpl.nasa.gov ; and

http://winds.jpl.nasa.gov

JPL is managed for NASA by the California Institute of Technology in Pasadena.

Alan Buis (818) 354-0474
Jet Propulsion Laboratory, Pasadena, Calif.

Tracey Bryant (302) 831-8185
University of Delaware, Newark

2006-040



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