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Seismic waves are converted into acoustic waves at the interface of the ground and the atmosphere. These acoustic waves contains information on the planet internal structure because they conserve the properties of seismic waves. Analyzing atmospheric waves is critical to infer the internal structure of planets with hot and dense atmosphere, where no ground instrument can be deployed over a long period. Pressure sensors on board stratospheric balloons can measure these acoustic waves produced by seismic waves. Such measurements were recently presented for two quakes detected by the balloons of the Stratéole-2 project (Garcia et al., 2022). However, this study does not model the relation between the ground displacements and the recorded pressure variations. Here we aim to fully understand the content of these data by comparing them to synthetic data. We model the seismic and acoustic waves with …