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Listening to the Ocean's Temperature
 

The 1998 North Pacific Acoustic Laboratory cruise (NPAL '98)
The 1998 North Pacific Acoustic Laboratory cruise (NPAL '98) aboard Scripp's R/V Melville involved deployment of instrument arrays essential to the Acoustic Thermometry of Ocean Climate (ATOC) experiment.

Map of a feasibility study of acoustic thermometry in the North Pacific Ocean.
Map of a feasibility study of acoustic thermometry in the North Pacific Ocean. Lines represent acoustic paths from sound sources on the U.S. West Coast and in Hawaii to U.S. Navy and other receivers. Paths cover distances of up to 3,100 miles (5,000 km) in the North Pacific, with a 6,200 mile (10,000 km) path to New Zealand. ATOC represents the first attempt to directly provide average measures of temperature throughout much of the Pacific Ocean basin.

Acoustic thermometry is a method that was devised for tracking long-term changes in ocean temperature by using low-frequency sounds transmitted across ocean basins at a particular depth. The technique, which works because the speed of sound is proportional to water temperature, was invented by Walter Monk at Scripps Institute of Oceanography and Carl Wunsch at Massachusetts Institute of Technology, with support from the Office of Science. It turns out that acoustic thermometry is a sensitive technique not only for measuring the average temperature of vast expanses of ocean but also for tracking long-term changes in ocean climate associated with global warming. The idea works by sending sound signals from underwater speakers and tracking how long it takes them to reach receivers moored to the ocean floor thousands of miles away. Because sound travels faster in warmer water; slower in cooler water, recording increasingly faster travel times of the sound waves would indicate the ocean is warming. The concept was proven about 10 years ago, when the Office of Science and several other agencies demonstrated that acoustic thermometry could generate high-fidelity global and basin scale ocean thermal data.

Scientific Impact: Acoustic thermometry is more sensitive than local measurements for tracking long-term trends in ocean temperature because it can detect changes in deep ocean areas that exhibit little, if any, seasonal or interannual variation. This technique reduces the time required to detect a trend in climate warming from several decades to as little as a decade.

Social Impact: Acoustic thermometry helps to improve the science base for societal decisions and policymaking with regard to human activities that contribute to global warming. It may also reveal information about other oceanographic phenomena, such as El Nino events, that have profound effects on climate.

Reference: Munk, W. and C. Wunsch, "Ocean Acoustic Tomography: a scheme for large scale monitoring. Deep Ocean Research 26: 123-161 (1979).

Munch, W. and C. Wunsch, "Observing the ocean in the 1990's: a scheme for large-scale monitoring," Phil. Trans. Roy. Soc., A307, 439-464 (1982).

URL: http://atocdb.ucsd.edu/

Technical Contact: Dr. Ari Patrinos, Associate Director for Biological and Environmental Research, 301-903-3251

Press Contact: Jeff Sherwood, DOE Office of Public Affairs, 202-586-5806

SC-Funding Office: Office of Biological and Environmental Research

http://www.science.doe.gov
Back to Decades of Discovery home Updated: March 2001

 

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