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Shock Waves01:16

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...
Sound as Pressure Waves01:17

Sound as Pressure Waves

Sound waves, which are longitudinal waves, can be modeled as the displacement amplitude varying as a function of the spatial and temporal coordinates. As a column of the medium is displaced, its successive columns are also displaced. As the successive displacements differ relatively, a pressure difference with the surrounding pressure is created. The gauge pressure varies across the medium.
The pressure fluctuation depends on the difference in displacements between the successive points in the...
Sound Waves: Interference00:53

Sound Waves: Interference

Sound waves can be modeled either as longitudinal waves, wherein the molecules of the medium oscillate around an equilibrium position, or as pressure waves. When two identical waves from the same source superimpose on each other, the combination of two crests or two troughs results in amplitude reinforcement known as constructive interference. If two identical waves, that are initially in phase, become out of phase because of different path lengths, the combination of crests with troughs...
Echo01:06

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...
Sound Intensity00:58

Sound Intensity

The loudness of a sound source is related to how energetically the source is vibrating, consequently making the molecules of the propagation medium vibrate. To measure the loudness of a source, the physical quantity of interest is the intensity. This is defined as the energy emitted per unit of time per unit of area perpendicular to the sound wave's propagation direction. Since the total energy is greater if the source vibrates for a longer duration and over a larger area, dividing the emitted...
Sound Waves: Resonance01:14

Sound Waves: Resonance

Resonance is produced depending on the boundary conditions imposed on a wave. Resonance can be produced in a string under tension with symmetrical boundary conditions (i.e., has a node at each end). A node is defined as a fixed point where the string does not move. The symmetrical boundary conditions result in some frequencies resonating and producing standing waves, while other frequencies interfere destructively. Sound waves can resonate in a hollow tube, and the frequencies of the sound...

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Computationally robust and noise resistant numerical detector for the detection of atmospheric infrasound.

The Journal of the Acoustical Society of America·2013
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Uncertainties associated with parameter estimation in atmospheric infrasound arrays.

The Journal of the Acoustical Society of America·2004
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Related Experiment Video

Updated: Jun 18, 2026

Blast Quantification Using Hopkinson Pressure Bars
09:41

Blast Quantification Using Hopkinson Pressure Bars

Published on: July 5, 2016

Explosion localization via infrasound.

Curt A L Szuberla, John V Olson, Kenneth M Arnoult

    The Journal of the Acoustical Society of America
    |November 10, 2009
    PubMed
    Summary
    This summary is machine-generated.

    A new meta-array technique significantly improves infrasound source localization precision. This method enhances accuracy compared to traditional back azimuth methods, offering an order of magnitude improvement in performance.

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    Area of Science:

    • Acoustics
    • Geophysics
    • Signal Processing

    Background:

    • Infrasonic data analysis is crucial for monitoring natural and anthropogenic events.
    • Traditional acoustic source localization relies on ensembles of small arrays and back azimuth calculations.
    • Existing methods face challenges in achieving high precision for low-frequency sources.

    Purpose of the Study:

    • To compare the performance of a novel meta-array technique against a standard back azimuth approach for infrasonic source localization.
    • To evaluate the precision improvements offered by the meta-array method.

    Main Methods:

    • Applied two acoustic source localization techniques to infrasonic data.
    • Compared a standard ensemble of small arrays method with a novel meta-array approach.
    • Validated techniques through numerical simulations and a field experiment using a 3-km-aperture meta-array.

    Main Results:

    • The meta-array technique demonstrated superior localization precision compared to the standard method.
    • Improvements in precision were observed across the vicinity of the meta-array.
    • Precision gains were often an order of magnitude greater with the meta-array approach.

    Conclusions:

    • The meta-array technique offers a significant advancement in infrasonic source localization.
    • This novel approach provides enhanced precision, particularly valuable for low-frequency acoustic monitoring.
    • The findings support the adoption of meta-array configurations for improved geophysical and acoustic sensing.