HIGHLIGHTS
- What: This study focuses on the acoustic wave modes to understand the origin of rapid CSTDs. The consistent ray-tracing simulation in this study validates the AGW energetics in altitude-varying sound profiles, as presented in Figures 2 and 3. The simulation of ionoquakes is beyond the scope of the present study, and the authors aim to present it in a separate study. The study aims to simulate co-seismic atmospheric disturbances, estimate their formation time at thermospheric heights, and compare these estimations with ray-tracing estimations.
- Who: Saul A. Sanchez and Esfhan A. Kherani . . .

If you want to have access to all the content you need to log in!
Thanks :)
If you don't have an account, you can create one here.