## 2. The basic equationsThe linearized hydrodynamic equations for adiabatic fluctuations, expressing the conservation of mass, momentum and internal energy for a gravitationally stratified, isothermal atmosphere can be written in the form: where , and are, respectively, the perturbed gas pressure and density and the velocity; the subscript 0 denotes the unperturbed variables; is the gravitational acceleration, is the sound speed and is the ratio of specific heats. The equilibrium values of unperturbed variables have the form: where and are, respectively, the values of pressure and density at the reference height ; and is the pressure scale height. In order to simplify the calculations it is convenient to assume the height dependence (see Lamb 1932) With these assumptions and measuring space in units of twice the pressure scale height, , and time in units of , where is the cutoff period, Eqs. (1) become where is any of the variables (2)
or (3) in non-dimensional form, i.e.,
,
and i.e. the `reduced'
perturbations, and and
are Laplacian operators. Note that
the reduced quantities We perform a plane-wave analysis assuming that all variables are proportional to . Eq. (4) then yields the dispersion relation (Bray & Loughhead 1974), where is in units of and in units of . Eq. (5) can be solved to obtain where the plus sign is for the two roots for The summation goes over four modes corresponding to the four roots of the dispersion relation (5), i.e., both acoustic and internal gravity modes travelling in two directions. In order to obtain the values of of Eqs. 8-10, i.e., the relation between density, velocities and pressure in the plane-wave solutions, we have Fourier analyzed system (1), derived a set of algebraic equations (Appendix A), and determined the amplitudes by matching the given initial conditions at (Appendix B). As initial conditions we have considered a pressure pulse; the set of conditions becomes: where is the amplitude of the initial perturbation and is the spatial width of the Gaussian. Note that this four conditions completely determine the solution since we have fourth order equation. The analytical form for the amplitudes is given in Appendix B. © European Southern Observatory (ESO) 2000 Online publication: January 31, 2000 |