Related Experiment Video
Updated: May 27, 2026

08:19
Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
Published on: May 9, 2021
The effect of wind-generated bubbles on sea-surface backscattering at 940 Hz
Robbert van Vossen1, Michael A Ainslie
1TNO, Oude Waalsdorperweg 63, P.O. Box 96864, 2509 JG The Hague, The Netherlands. robbert.vanvossen@tno.nl
The Journal of the Acoustical Society of America
|November 18, 2011
Summary
Predictions of sea-surface backscattering strength are challenging at low frequencies. This study shows that scattering from individual resonant bubbles, not just bubble clouds, can explain sonar performance data.
Area of Science:
- Ocean acoustics
- Acoustic scattering
- Sonar performance modeling
Background:
- Sea-surface backscattering strength predictions are crucial for sonar performance.
- Measurements at small grazing angles relevant to low-frequency active sonar (1-3 kHz) are scarce.
- Understanding scattering mechanisms is key for accurate theoretical predictions.
Purpose of the Study:
- To investigate individual resonant bubbles as a sea-surface backscattering mechanism.
- To develop a scattering model incorporating resonant bubbles and rough surface scattering.
- To validate the model against Critical Sea Test (CST) measurements.
Main Methods:
- Derived a theoretical scattering model including individual resonant bubbles.
- Incorporated rough surface scattering into the model.
- Fitted model results to CST measurements at 940 Hz, parameterizing large bubble concentration.
Main Results:
- The model successfully explains CST data.
- A small number of large resonant bubbles can account for the observed scattering.
- This indicates resonant bubbles are a significant alternative to bubble clouds.
Conclusions:
- Individual resonant bubbles represent a viable mechanism for sea-surface backscattering at low frequencies.
- The developed model provides a new tool for sonar performance prediction.
- Further research should explore the prevalence and impact of resonant bubbles in various sea states.
Related Concept Videos
Echo
The human ear cannot distinguish between two sources of sound if they happen to reach within a specific time interval, typically 0.1 seconds apart. More than this, and they are perceived as separate sources.
Imagine the sound is reflected back to the ears. Assuming that the source is very close to the human, the difference between hearing the two sounds—the emitted sound and the reflected sound—may be more than the minimum time for perceiving distinct sounds. If this is the case, then the...
Imagine the sound is reflected back to the ears. Assuming that the source is very close to the human, the difference between hearing the two sounds—the emitted sound and the reflected sound—may be more than the minimum time for perceiving distinct sounds. If this is the case, then the...
Deriving the Speed of Sound in a Liquid
As with waves on a string, the speed of sound or a mechanical wave in a fluid depends on the fluid's elastic modulus and inertia. The two relevant physical quantities are the bulk modulus and the density of the material. Indeed, it turns out that the relationship between speed and the bulk modulus and density in fluids is the same as that between the speed and the Young's modulus and density in solids.
The speed of sound in fluids can be derived by considering a mechanical wave propagating...
The speed of sound in fluids can be derived by considering a mechanical wave propagating...
Shock Waves
While deriving the Doppler formula for the observed frequency of a sound wave, it is assumed that the speed of sound in the medium is greater than the source's speed through it. When this condition is breached, a shock wave occurs.
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high pressures...
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high pressures...
Doppler Effect - II
The Doppler effect has several practical, real-world applications. For instance, meteorologists use Doppler radars to interpret weather events based on the Doppler effect. Typically, a transmitter emits radio waves at a specific frequency toward the sky from a weather station. The radio waves bounce off the clouds and precipitation and travel back to the weather station. The radio frequency of the waves reflected back to the station appears to decrease if the clouds or precipitation are moving...
Propagation of Waves
When a wave propagates from one medium to another, part of it may get reflected in the first medium, and part of it may get transmitted to the second medium. In such a case, the interface of the two mediums can be considered as a boundary that is neither fixed nor free.
Consider a scenario where a wave propagates from a string of low linear mass density to a string of high linear mass density. In such a case, the reflected wave is out of phase with respect to the incident wave, however the...
Consider a scenario where a wave propagates from a string of low linear mass density to a string of high linear mass density. In such a case, the reflected wave is out of phase with respect to the incident wave, however the...
Reflection of Waves
When a wave travels from one medium to another, it gets reflected at the boundary of the second medium. A common example of this is when a person yells at a distance from a cliff and hears the echo of their voice. The sound waves (longitudinal waves) traveling in the air are reflected from the bounding cliff. Similarly, flipping one end of a string whose other end is tied to a wall causes a pulse (transverse wave) to travel through the string, which gets reflected upon reaching the wall. In...

