Researchers and crew aboard R/V Melville deploy an acoustic recording package off Kauai. The acoustic properties of the seas just west of the island were the subject of a nearly month-long study led by Scripps.
The Secrets of Effective Communication
In turbulent seas off Kauai, Scripps researchers measure the physical properties that stand in the way of successful underwater acoustic data transmissions
An acoustic signal is sent horizontally through ocean waters from one point to another. Along the way the sound is bouncing off a “ceiling” of choppy, wind-whipped seas and seafloor that could be craggy rock or smooth sand.
If researchers can better understand how physical conditions like these distort sound as it travels through the ocean, they could send data underwater faster and with less power and could make it much easier for networks of sensors to talk to each other simultaneously. They could improve wireless communications from commonly used ocean instruments such as Doppler current profilers and potentially eliminate the need for vehicles and gliders to surface just to transmit modest amounts of data.
With these goals on the horizon, a science team led by Scripps Institution of Oceanography at UC San Diego researchers completed in July a three-week study of waters west of the Hawaiian island of Kauai. Scripps acoustician Bill Hodgkiss, principal investigator of the project known as the Kauai Acomms Multidisciplinary University Research Initiative (MURI) Experiment, said the region was chosen for its dynamic characteristics.
“It goes from very calm to whitecap conditions every 24 hours and that repeats on a regular basis,” Hodgkiss said.
The research team, which included Scripps researchers Bill Kuperman, Heechun Song, and Bruce Cornuelle, and colleagues from UCSD, the University of Delaware, and Arizona State University, inventoried the suite of conditions that can disrupt a signal as it travels between two underwater points. The team recorded wind speed and surface wave measurements to gauge the structure of the sea surface and temperature profiles to estimate sound speed (the colder the water, the slower sound travels), and measured the topography of the seafloor.
Hodgkiss rated the experiment a major success and said its data could enhance computer models used to guide development of underwater acoustic modems-especially for use in places less accessible than Kauai.
“This experiment should improve prediction of the fluctuation characteristics in other environments that scientists don't necessarily have the resources to go and study,” Hodgkiss said.
—Robert Monroe
September 2008
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