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Amplitude<br />

Table A1. The speed of sound (m/s) in various media, from JASCO Applied Sci<strong>en</strong>ces (2009).<br />

Medium<br />

Speed of sound in m/s<br />

Air at 20 o C 343<br />

Salt water at 25 o C 1532<br />

Sand 800-2,200<br />

Clay 1,000-2,500<br />

Sandstone 1,400-4,300<br />

Granite 5,500-5,900<br />

Limestone 5,900-6,100<br />

How do we describe sound?<br />

Laypeople typically describe a sound by its loudness, and sometimes its pitch. The criteria that<br />

determine these characteristics are basically the sound wave’s amplitude (loudness), frequ<strong>en</strong>cy (pitch),<br />

and duration. Waveforms are used to show time vs. amplitude (Figures A1-2), and spectrograms show<br />

time vs frequ<strong>en</strong>cy, much like a musical score (Figure A3). Continuous sounds such as boat noise are<br />

described as chronic or non-pulsed whereas sounds that are of short duration, such as an explosion, or<br />

of repeated short durations, such as pile driving or airgun firing, are pulsed (or acute, intermitt<strong>en</strong>t or<br />

transi<strong>en</strong>t) sources of noise. In the Atlantic Ocean, airgun firing is such a predominant sound that it is<br />

oft<strong>en</strong> described as chronic because it is ever-pres<strong>en</strong>t, but the original signal is a pulsed sound. Sounds<br />

such as killer whale whistles or military sonars are g<strong>en</strong>erally described as narrowband, whereas sounds<br />

that <strong>en</strong>compass a range of frequ<strong>en</strong>cies, such as shipping noise or pile driving, are broadband (Figure A3).<br />

1<br />

0.5<br />

a) Low frequ<strong>en</strong>cy: 3 cycles/s (Hz) b) higher frequ<strong>en</strong>cy: 6 cycles/s (Hz)<br />

1<br />

0.5<br />

0<br />

0<br />

-0.5<br />

-0.5<br />

-1<br />

-1<br />

0 1 0 1<br />

Time (s)<br />

Figure A1. Waveforms of a low (a) and higher (b) frequ<strong>en</strong>cy continuous sound wave.<br />

74

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