io of specific heats ‘γ’</li>
<li>atmospheric pressure ‘p₀’ in Pa</li>
<li>density of water ‘ρ’ in kg/m³</li>
<li>acceleration due to gravity ‘g’ in m/s²</li>
</ul>
<p>This ignores surface-tension, thermal, viscous and acoustic damping effects, and the pressure-volume relationship is taken to be adiabatic. Implementation based on Medwin &amp; Clay (1998).</p>
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