EGU23-16759, updated on 26 Feb 2023
https://doi.org/10.5194/egusphere-egu23-16759
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ionospheric Hole in the MLT Regions after Submarine Volcanic Eruptions

Sovit Khadka1, Cesar Valladares2, and Andrew Gerrard1
Sovit Khadka et al.
  • 1New Jersey Institute of Technology, Center for Solar-Terrestrial Research, Newark, United States of America (khadka@njit.edu)
  • 2The University of Texas at Dallas, Richardson, TX 75080 (Cesar.Valladares@utdallas.edu)

A gigantic submarine volcano erupted near Tonga Island on 15 January 2022 generating a tsunami and related atmospheric and oceanic waves across the globe. This violent volcano triggered extreme disturbances just above the volcanic center that reached near Earth’s stratosphere. This geophysical event generated acoustic-gravity waves to propagate upward and induce significant global perturbations and holes in the mesosphere and lower thermosphere (MLT) regions. Here, we study the MLT region’s response to the Tonga-induced perturbations using ground-based Global Positioning System (GPS)-total electron content (TEC) data from GPS receivers spread in the South American continent. The possible propagation mechanism of the Tonga-related ionospheric holes and perturbations mediated by neutral wind-driven dynamo fields, vertical drifts, and the contribution of geomagnetic conditions will also be discussed. 

How to cite: Khadka, S., Valladares, C., and Gerrard, A.: Ionospheric Hole in the MLT Regions after Submarine Volcanic Eruptions, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-16759, https://doi.org/10.5194/egusphere-egu23-16759, 2023.