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=====Set the Surface Pressure Fluctuation to Zero===== Using the [[#PGE:AdiabaticFirstLaw|above "Linearized Adiabatic Form of the First Law of Thermodynamics"]] to replace the fractional density variation, <math>~d</math>, in favor of the fractional pressure variation, <math>~p</math> in the [[#Continuity|above "Linearized Equation of Continuity"]], gives, <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~p</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~-\gamma_g \biggl( 3 x + r_0 \frac{dx}{dr_0} \biggr) \, .</math> </td> </tr> </table> </div> [http://adsabs.harvard.edu/abs/1941ApJ....94..124L Ledoux & Pekeris (1941]; see [[#Ledoux_and_Pekeris_.281941.29|additional discussion below]]) suggest that an adequate outer boundary condition is provided by setting the fractional pressure fluctuation, <math>~p</math>, to zero at the surface. Leaning on this just-derived relation, therefore, they recommend (see their equation 4) imposing the following surface boundary constraint on the fractional radial variation, <math>~x</math>: <div align="center"> <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~-\gamma_g \biggl( 3 x + r_0 \frac{dx}{dr_0} \biggr)</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~0</math> at <math>~r_0 = R \, .</math> </td> </tr> </table> </div>
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