Harriet George

Postdoctoral researcher


Curriculum vitae



Laboratory for Atmospheric and Space Physics

University of Colorado Boulder



Cosmic noise absorption signature of particle precipitation during ICME sheaths and ejecta


Journal article


E. Kilpua, L. Juusola, M. Grandin, A. Kero, S. Dubyagin, N. Partamies, A. Osmane, H. George, M. Kalliokoski, T. Raita, T. Asikainen, M. Palmroth
2019

Semantic Scholar DOI
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APA   Click to copy
Kilpua, E., Juusola, L., Grandin, M., Kero, A., Dubyagin, S., Partamies, N., … Palmroth, M. (2019). Cosmic noise absorption signature of particle precipitation during ICME sheaths and ejecta.


Chicago/Turabian   Click to copy
Kilpua, E., L. Juusola, M. Grandin, A. Kero, S. Dubyagin, N. Partamies, A. Osmane, et al. “Cosmic Noise Absorption Signature of Particle Precipitation during ICME Sheaths and Ejecta” (2019).


MLA   Click to copy
Kilpua, E., et al. Cosmic Noise Absorption Signature of Particle Precipitation during ICME Sheaths and Ejecta. 2019.


BibTeX   Click to copy

@article{e2019a,
  title = {Cosmic noise absorption signature of particle precipitation during ICME sheaths and ejecta},
  year = {2019},
  author = {Kilpua, E. and Juusola, L. and Grandin, M. and Kero, A. and Dubyagin, S. and Partamies, N. and Osmane, A. and George, H. and Kalliokoski, M. and Raita, T. and Asikainen, T. and Palmroth, M.}
}

Abstract

Abstract. We study here energetic (E > 30 keV) electron precipitation using cosmic noise absorption (CNA) during the sheath and ejecta structures of 61 interplanetary coronal mass ejections (ICMEs) observed in the near-Earth solar wind between 1997 and 2012. The data comes from the Finnish riometer chain from stations extending from auroral (IVA, 65.2 geomagnetic latitude, MLAT) to subauroral (JYV, 59.0 MLAT) latitudes. We find that sheaths and ejecta lead frequently to enhanced CNA (> 0.5 dB) both at auroral and subauroral latitudes, although the CNA magnitudes stay relatively low (medians around 1 dB). Due to their longer duration, ejecta typically lead to more sustained enhanced CNA periods (on average 6–7 hours), but the sheaths and ejecta were found to be equally effective in inducing enhanced CNA when relative occurrence frequency and CNA magnitude were considered. Only at the lowest MLAT station JYV ejecta were more effective in causing enhanced CNA. Some clear magnetic local time (MLT) trends and differences between the ejecta and sheath were found. The occurrence frequency and magnitude of CNA activity was lowest close to midnight, while it peaked for the sheaths in the morning and afternoon/evening sectors and for the ejecta in the morning and noon sectors. These differences may reflect differences in typical MLT distributions of wave modes that precipitate substorm-injected and trapped radiation belt electrons during the sheath and ejecta. Our study also emphasizes the importance of substorms and magnetospheric ULF waves for enhanced CNA.


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