Articles | Volume 44, issue 2
https://doi.org/10.5194/angeo-44-881-2026
https://doi.org/10.5194/angeo-44-881-2026
Regular paper
 | 
01 Sep 2026
Regular paper |  | 01 Sep 2026

Magnetotail response to corotating interaction region driven geomagnetic storms: Cluster observations

Adriane Marques de Souza Franco, Rashmi Rawat, Mauricio José Alves Bolzan, and Ezequiel Echer

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Cited articles

Abbo, L., Ofman, L., Antiochos, S. K., Hansteen, V. H., Harra, L., Ko, Y.-K., Lapenta, G., Li, B., Riley, P., Strachan, L., von Steiger, R., and Wang, Y.-M.: Slow solar wind: Observations and modeling, Space Sci. Rev., 201, 55–108, https://doi.org/10.1007/s11214-016-0264-1, 2016. 
Alves, M., Echer, E., and Gonzalez, W.: Geoeffectiveness of corotating interaction regions as measured by Dst index, J. Geophys. Res.-Space, 111, A07S05, https://doi.org/10.1029/2005JA011379, 2006. 
Antonova, E. E. and Stepanova, M. V.: The impact of turbulence on physics of the geomagnetic tail, Frontiers in Astronomy and Space Sciences, 8, 622570, https://doi.org/10.3389/fspas.2021.622570, 2021. 
Baumjohann, W. and Nakamura, R.: Magnetospheric contributions to the terrestrial magnetic field, Developments in Earth and Environmental Sciences, 5, 77–92, https://doi.org/10.1016/B978-044452748-6.00088-2, 2007. 
Bolzan, M. J. A.: Statistical and wavelet analysis of the solar wind data, Braz. J. Phys., 35, 592–596, https://doi.org/10.1590/S0103-97332005000400002, 2005. 
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Short summary
This study investigates 40 geomagnetic storms driven by corotating interaction regions and their impact on Earth's magnetotail. We find that short, 4 h energy pulses dominate the magnetotail during cyclic substorms. Furthermore, High-Intensity, Long-Duration, Continuous Auroral Activity (HILDCAA) events in the recovery phase facilitate energy distribution across 2–12 h periodicities in the auroral region. Spectral indices indicate strong turbulence in both regions.
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