EGU25-2283, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-2283
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 02 May, 14:25–14:35 (CEST)
 
Room 1.15/16
On the Ionosphere-Atmosphere-Lithosphere coupling during theNovember 9, 2022 Italian Earthquake
Mirko Piersanti1,2,3, Giulia D'Angelo1,2, Dario Recchiuti4,2, Fabio Lepreti5, Paola Cusano6, Enza De Lauro7, Vincenzo Carbone5, Pietro Ubertini2, and Mariarosaria Falanga7
Mirko Piersanti et al.
  • 1University of L'Aquila, Department of Physical and Chemical Sciences, L'Aquila, Italy (mirko.piersanti@univaq.it)
  • 2National Institute of Astrophysics, IAPS, Rome, Italy.
  • 3INFN, sezione di Roma "Tor Vergata", Rome, Italy.
  • 4University of Trento, Department of Physics, Trento, Italy.
  • 5Università della Calabria, Dipartimento di Fisica, Rende, Cosenza, Italy.
  • 6Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli, Naples, Italy
  • 7University of Salerno, Department of Information and Electric Engineering and Applied Mathematics, Fisciano, Salerno, Italy

In the last decades, the scientific community has been focused on searching earthquake signatures in the Earth's atmosphere, ionosphere, and magnetosphere. This work investigates an offshore Mw 5.5 earthquake that struck off the Marche region's coast (Italy) on November 9, 2022, with a focus on the potential coupling between the Earth's lithosphere, atmosphere, and magnetosphere triggered by the seismic event. Analysis of atmospheric temperature data from ERA5 reveals a significant increase in potential energy (Ep) at the earthquake's epicenter, consistent with the generation of Atmospheric Gravity Waves (AGWs). This finding is further corroborated by the MILC analytical model, which accurately simulates the observed Ep trends (within 5%), supporting the theory of Lithosphere-Atmosphere-Ionosphere-Magnetosphere Coupling. The study also examines the vertical Total Electron Content (vTEC) and finds notable fluctuations at the epicenter, exhibiting periodicities (7-12 minutes) characteristic of AGWs and traveling ionospheric disturbances. The correlation between ERA5 observations and MILC model predictions, particularly in temperature deviations and Ep distributions, strengthens the hypothesis that earthquake-generated AGWs impacted atmospheric conditions at high altitudes, leading to observable ionospheric perturbations. This research contributes to a deeper understanding of Lithosphere-Atmosphere-Ionosphere-Magnetosphere Coupling mechanisms and the potential for developing reliable earthquake prediction tools.

How to cite: Piersanti, M., D'Angelo, G., Recchiuti, D., Lepreti, F., Cusano, P., De Lauro, E., Carbone, V., Ubertini, P., and Falanga, M.: On the Ionosphere-Atmosphere-Lithosphere coupling during theNovember 9, 2022 Italian Earthquake, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-2283, https://doi.org/10.5194/egusphere-egu25-2283, 2025.