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This Standard provides the means to calculate atmospheric absorption losses of sound from any source, moving or stationary, for a wide range of meteorological conditions. The atmosphere is assumed to be still, homogeneous moist air of normal composition. Non-homogeneous atmospheres may be divided into horizontal layers within which homogeneous conditions may be assumed. Attenuation coefficients for pure-tone sounds are calculated by means of equations (or a table) over ranges of frequency, and the humidity, pressure, and temperature of the atmosphere. For sounds analyzed by fractional-octave- band filters (e.g., one-third-octave- band filters), alternative methods are provided in annexes to calculate the attenuation caused by atmospheric absorption from that specified for pure- tone sounds.
 

Document History

  1. ASA S1.26-2014 (R2024)


    American National Standard Method for the Calculation of the Absorption of Sound by the Atmosphere

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  2. ASA S1.26-1995 (R2009)

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    American National Standard Method for the Calculation of the Absorption of Sound by the Atmosphere

    • Historical Version