Acoustic techniques used by MIT researchers to explore the Arctic Ocean may help determine whether there is a vast liquid ocean under the ice blanketing Europa, one of Jupiter's moons.
The researchers reported at the Chicago meeting of the Acoustical Society of America on June 5 that they may be able to use a technique similar to ultrasound or the sonar navigation used by bats and dolphins to gather information about Europa.
Professor of Ocean Engineering Nicholas C. Makris said implanting soda can-sized sensors in Europa's icy exterior could provide researchers with information on the temperature and structure of the planet. Current sensor technology makes it possible to detect even tiny motions, and there is evidence that massive ice fractures on Europa's surface occur daily.
While such an experiment may be a decade or more away, this unconventional approach to planetary exploration would have to begin to be developed now, Professor Makris said. An array of geophones on the icy surface could simultaneously localize discrete events such as fractures and determine the moon's ice-layer thickness as well as the thickness of a potential ocean layer.
SEARCHING FOR WATER
Europa may be the only entity in our solar system besides Earth that contains a great deal of water, researchers say, and this mission would represent the first time ocean scientists have been involved in planetary exploration.
Gravity and magnetic data collected by the NASA Galileo Orbiter over the past five years have provided increasing evidence that an ocean exists underneath Europa's uniform, 10- to 100-kilometer thick coat of ice. The possible ocean on Europa may contain more liquid water than all the oceans on Earth combined.
Magnetic studies have indicated that there must be a conducting layer in Europa. A salty ocean would fit the bill. Researchers hope to discover whether Europa is made up entirely of mushy ice or if it contains an ocean. And where there is water, there may be life.
USING SOUND TO 'SEE'
Pictures of the moon show odd, cusp-shaped cracks in the surface. Europa's numerous fractures and ridges are believed to have formed in response to tidal deformations generated by the moon's slightly eccentric 85-hour orbit around Jupiter.
Inspired by evidence for these regularly occurring ice fractures, the MIT researchers propose probing Europa's interior by deploying an array of surface microphones that listen to naturally occurring sound. Knowledge of ice mechanics suggest that these propagating fractures would generate significant acoustic energy in the frequency range 0.1 to 100 Hz.
Studying the ice sounds would allow researchers to see if there was a connection between the moon's orbital period and the ice fractures, which occur on Europa once every 30 seconds. Meteors hit Europa about once a month, and these also could be used as sound sources.
AN ARCTIC EXPLORATION
Researchers led by Dr. Makris, the Doherty Professor of Ocean Utilization, have used sound-based techniques to explore the Arctic Ocean. By inserting vibration-sensitive hydrophones in the water, they used ambient sound to listen for changes in noise levels and found that noise levels increased when winds and currents put stresses on the ice.
"Noise levels are like a thermometer for stress on the ice," Professor Makris said. "The ice is very sensitive and conducive to sound." Sound waves made by large fractures go through the ice and penetrate into the ocean.
These low-frequency sound waves, akin to those created by whales, get trapped and can propagate hundreds of kilometers through the water. Even if they can't be heard, instruments can pick up their vibrations from a distance.
In addition to Professor Makris, the research team includes ocean engineering postdoctoral associates Aaron M. Thode and Michele Zanolin, and graduate students Yi-San Lai, Sunwoong Lee, Purnima Ratilal and Joshua Wilson.
This work is funded by the Office of Naval Research. Professor Makris is the Secretary of the Navy/Chief of Naval Operations Scholarof Oceanographic Sciences.
A version of this article appeared in MIT Tech Talk on June 6, 2001.
