EGU24-2428, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-2428
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Pc 4 Cavity mode wave frequency variation associated with inward motion of the magnetopause during interplanetary shock compression

Dianjun Zhang1,2, Wenlong Liu1,2, Zhao Zhang1,2, Xinlin Li3, Theodore Sarris3,4, Jerry Goldstein5,6, and Rezvov Dmitry7
Dianjun Zhang et al.
  • 1School of Space and Environment, Beihang University, Beijing, China
  • 2Key Laboratory of Space Environment Monitoring and Information Processing of MIIT, Beihang University, Beijing, China
  • 3Laboratory for Atmospheric and Space Physics, University of Colorado Boulder, Boulder, CO, USA
  • 4Department of Electrical and Computer Engineering, Democritus University of Thrace, Xanthi, Greece
  • 5Space Science and Engineering Division, Southwest Research Institute, San Antonio, Texas, USA
  • 6Department of Physics and Astronomy, University of Texas San Antonio, Texas, USA
  • 7Arctic and Antarctic Research Institute, St.Petersburg, Russia

A cavity mode wave, referring to a trapped or radially standing fast mode wave between different magnetospheric boundaries, has been developed in theory and reported in observation studies. In this study, we present an interplanetary shock (IPS)-induced cavity mode wave event observed outside the plasmasphere on 31 August 2017 with multispacecraft measurements. The phase delay of 90 degrees between the azimuthal electric field and compressional magnetic field indicates that the fast-mode wave triggered by the IPS is a standing wave, presumably radially trapped in the cavity between the magnetopause and plasmapause. Taking advantage of the location of VAP-B spacecraft right outside the plasmapause and the AARI ground-based high-latitude array mapped in the noon sector, it is suggested that the observed compressional wave associates to cavity mode with its inner boundary at the plasmapause and its outer boundary at the magnetopause. The peak frequency of the wavelet spectrum of the compressional magnetic field increases from 10.5 to 12.5 mHz, which is consistent with the theoretically calculated cavity eigenfrequencies before and after the IPS. We also provide the first evidence that the peak frequency of the cavity mode increases due to the inward motion of the magnetopause during IPS compression.

How to cite: Zhang, D., Liu, W., Zhang, Z., Li, X., Sarris, T., Goldstein, J., and Dmitry, R.: Pc 4 Cavity mode wave frequency variation associated with inward motion of the magnetopause during interplanetary shock compression, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2428, https://doi.org/10.5194/egusphere-egu24-2428, 2024.