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Wave propagation in idealized stellar atmospheres is modeled by the equations of ideal MHD, together with the gravity source term.
In this paper we will present and analyze a new class of the IMEX finite volume schemes for the Euler equations with a gravity source term.
Local hydrostatic reconstructions and suitable discretization of the gravity source term lead to a well-balanced scheme, i.e., a scheme which exactly preserves a discrete version of the relevant steady states.
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This technique gives the geographic positions and the depth of gravity sources.
This operation accentuates the effect of deep gravity sources and attenuates or even removes the influence of the superficial ones (Jacobsen 1987; Marcel et al. 2016; Abate Essi et al. 2017).
A new convective gravity wave source spectrum parameterization has been implemented in the Whole Atmosphere Community Climate Model version 2 (WACCM2).
In Newtonian gravity, the source is mass.
Without knowing anything else about them, we can assume that charge (in the case of electromagnetism) and mass (in the case of gravity) are sources of forces that act at infinitely large distances.
The latter is sometimes called "parameterization of gravity wave sources".
This trend is evident in the compiled gravity profiles sourced from Danis et al. (2011) used to define basin geometry at a relatively high spatial resolution.
A ray tracing technique was applied in order to find out the gravity wave sources and to investigate the propagation of these waves through the atmosphere.
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