How is sound used to measure global climate change?

One way the ocean will respond to global climate change is with a change in temperature. The average temperature of the ocean will rise as global climate warms. Where the warming occurs and the rate at which it occurs are of great interest to climatologists. There are several difficulties in measuring the kinds of temperature changes that interest climatologists.

  1. The ocean is very large. To get a good picture of temperature change in the ocean, measurements of the whole ocean are needed.
  2. The ocean is filled with warm and cold eddies, similar to storms in the atmosphere. The temperature changes associated with these eddies are large compared to the small changes in ocean temperature expected from climate change. Large-scale average temperatures are needed to see climate change.
  3. The temperature measurements must be continuous in time.

All of these requirements mean that lowering temperature sensors from ships will not provide the kind of information on climate change that is needed. Although measurements made by lowering a temperature sensor from a ship are very accurate, many such measurements must be combined to provide the large-scale averages needed to see climate change. There are simply not enough ships to make continuing measurements of temperature all over the ocean.

Satellite measurements will help, but they only provide information at the ocean surface. Measurements made by drifting buoys that send data back by satellite will also help (http://www.argo.ucsd.edu/), but data from many buoys will have to be averaged. Using sound to measure ocean temperatures directly provides the large-scale average temperatures needed to study climate change (http://atoc.ucsd.edu/, http://npal.ucsd.edu/).

In warmer water, sound travels faster. By measuring the travel time of sound between two points, the average temperature of the water between those points can be determined. Very precise measurements of the average temperature can be made with sound.

Acoustic tomography can be used to measure the temperature of the ocean over large areas. A sound source sends out a sound signal at known times. The sound is sent out in the SOFAR channel so that it will travel as far as possible. Low-frequency sound can travel thousands of kilometers in the ocean. Hydrophones all over the ocean basin listen for the sound. The time taken to travel to each hydrophone is then calculated and the average temperature determined. The results apply to large areas of the ocean, necessary for understanding climate change.

Diagram showing a network of hydrophones used to measure the temperature of the ocean over a large area (acoustic tomography).

The time taken to travel to the hydrophone can be measured to within 20-30 milliseconds (20-30 thousandths of a second) at ranges of up to 5000 kilometers. The travel time over 5000 kilometers (3100 miles) is about an hour. This travel time accuracy lets us determine the average temperature to within a few millidegress (thousands of a degree) Celsius. Changes in travel time are due to changes in ocean temperature. The change in temperature can be measured to within 0.001 degrees Celsius per day. The ATOC (Acoustic Thermometry of Ocean Climate) project measured average temperatures in the North Pacific Ocean, for example, along a number of paths. Acoustic sources off central California and north of Kauai transmitted to U. S. Navy receivers, giving a sparse network of acoustic paths. They observed large-scale seasonal changes in ocean temperature of up to 2 degrees Celsius. This test verified that the technique does work. Transmissions continuing for many years could be used to measure large-scale climate change in the ocean. Transmissions are continuing from the ATOC source north of Kauai as part of the NPAL (North Pacific Acoustic Laboratory) program.

Image displaying sound sources and receivers used to measure Pacific Ocean surface temperatures.
This image displays sound sources and receivers (white dots) used to measure Pacific Ocean surface temperatures. The colors represent water depth. Reprinted with permission from Worcester, P.F. and R.C. Spindel, 2005: North Pacific Acoustic Laboratory. Journal of the Acoustical Society of America 117: 1499-1510. Copyright 2005, Acoustical Society of America.

The sound sources used in the ATOC and NPAL projects do not make a sound all the time. They typically make sound for 20 minutes every 4 hours on every fourth day. This results in six 20 minute transmissions for a total of 2 hours every 4 days. The sources send a sound out at a frequency centered on 75 Hz with a bandwidth of 35 Hz (the sound then has a frequency range of 57-92 Hz). The ATOC project used a low frequency because low frequencies travel further in the ocean than high frequencies.

You can listen to this sound below. You will need headphones or external speakers on your computer to hear the sound (75Hz is too low a frequency for most built in speakers). This recording of the ATOC source north of Kauai was amplified so you can hear it better.

Click either choice below to hear the ATOC Transmission:
You may need headphones or external speakers on your computer to hear this particular sound
 
Click this button use any media player
This recording is of the sound produced by the ATOC sound source at 75 Hz. This recording of the ATOC source was amplified so you can hear it better. You may need headphones or external speakers on your computer to hear this particular sound
From Scripps Institution of Oceanography
Additional Links on DOSITS

Additional Resources

  • "Able Sea Chicks Blog." (Link)
  • "Acoustic Thermometry of Ocean Climate (ATOC)" (Link)
  • "ARGO array (drifting buoys)" (Link)
  • "ATOC Project Homepage." (Link)
  • "North Pacific Acoustic Laboratory (NPAL)" (Link)
  • Spindel, R.C., and P.F. Worcester 1990, "Ocean acoustic tomography." Scientific American, 263, 94-99 (October, 1990) 
  • National Academy of Sciences, "Sounding Out the Oceans Secrets." (Link)