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Analysis and Ranking of the Acoustic Disturbance Potential of ...

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Report No. 6945<br />

BBN Systems <strong>and</strong> Technologies Corporation<br />

Ts is <strong>the</strong> time duration <strong>of</strong> a single sequence<br />

T is <strong>the</strong> time duration <strong>of</strong> <strong>the</strong> exposure period.<br />

P<br />

If a time-varying source produces most <strong>of</strong> its output within 5 dB <strong>of</strong> <strong>the</strong> maximum<br />

level, even though its output sequences are not identical, Eq. 7 may be<br />

simplified to <strong>the</strong> form:<br />

L = Lm + 10 Log (Tm/T )<br />

e q<br />

P<br />

where Lm is <strong>the</strong> median level <strong>of</strong> <strong>the</strong> highest exposure class<br />

Tm is <strong>the</strong> total time during which <strong>the</strong> exposure level was within k2.5 dB<br />

<strong>of</strong> Lm during <strong>the</strong> exposure period.<br />

(Note that for this case, <strong>the</strong> time ratio - T,/Tp.)<br />

3.1.3 Source spatial characterization<br />

Man-made noise is <strong>of</strong>ten produced by a moving source. A st<strong>and</strong>ard procedure<br />

has been established to determine <strong>the</strong> effective source output with<br />

respect to receiver locations which may be ei<strong>the</strong>r fixed or moving. This is<br />

done by measuring <strong>the</strong> source output at a st<strong>and</strong>ard reference range. The<br />

resulting sound level spectrum is called <strong>the</strong> source level (Ls) <strong>and</strong> is usually<br />

specified at a range <strong>of</strong> 1 m. For many sources which are too large to measure<br />

accurately at a range <strong>of</strong> 1 m, <strong>the</strong> local transmission loss is calibrated so<br />

measurements made at greater ranges can be corrected to an effective range <strong>of</strong><br />

1 m. For aircraft noise measurements where atmospheric absorption is an<br />

important factor in addition to <strong>the</strong> geometric spreading loss, it is customary<br />

to use a flyover altitude <strong>of</strong> 1000 ft (300 m) as a reference range to avoid<br />

large potential errors in estimating atmospheric absorption loss corractions<br />

back to a range <strong>of</strong> 1 m.<br />

From <strong>the</strong> viewpoint <strong>of</strong> a stationary listener, a moving source becomes a<br />

source with a,fluctuating output level even though <strong>the</strong> actual output <strong>of</strong> <strong>the</strong><br />

source may be constant. As a result <strong>the</strong> procedures developed in this report<br />

for application to fluctuating sources will also be relevant for use with<br />

moving sources. Source level spectra for sources which are usually moving are<br />

based on measurements made at <strong>the</strong> time <strong>of</strong> <strong>the</strong> closest point <strong>of</strong> approach (CPA)<br />

<strong>and</strong> range corrected using <strong>the</strong> CPA distance.<br />

3.2 Natural Background Noise<br />

There is a very large volume <strong>of</strong> literature on <strong>the</strong> subject <strong>of</strong> natural<br />

background noise (ambient ~oise) for both deep ocean <strong>and</strong> shallow water.<br />

Studies <strong>of</strong> ambient noise have ranged from treatments <strong>of</strong> specific environments<br />

(e.g., open ocean, isl<strong>and</strong> areas, harbors, near-shore or coastal regions <strong>and</strong><br />

arctic regions) to concern with underst<strong>and</strong>ing specific source characteristics<br />

<strong>and</strong> physical mechanisms. Classical references on <strong>the</strong> subject are Knudsen et<br />

a1 . ( 19441, Wenz ( 1962) <strong>and</strong> Ur ick ( 1983) . As one might expect, many causes <strong>of</strong>

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