Laboratory experiment to investigate the impact of background plasma on cyclotron emission

The auroral density cavity (a region of partial plasma depletion situated at an altitude of around 3200km at the Earth's pole) has been studied to have a background plasma density ~10 6 m -3 , and plasma frequency ~9kHz. Auroral Kilometric Radiation (AKR) is produced when particles descend thro...

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Published in2012 Abstracts IEEE International Conference on Plasma Science p. 2P-71
Main Authors McConville, S. L., King, M., Matheson, K., Whyte, C. G., Speirs, D. C., Gillespie, K. M., Phelps, A. D. R., Cross, A. W., Robertson, C. W., Ronald, K., Koepke, M. E., Cairns, R. A., Vorgul, I., Bingham, R., Kellett, B. J.
Format Conference Proceeding
LanguageEnglish
Published IEEE 01.07.2012
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Abstract The auroral density cavity (a region of partial plasma depletion situated at an altitude of around 3200km at the Earth's pole) has been studied to have a background plasma density ~10 6 m -3 , and plasma frequency ~9kHz. Auroral Kilometric Radiation (AKR) is produced when particles descend through this region and are magnetically compressed as they approach the Earth's magnetosphere and through conservation of the magnetic moment, a horseshoe shaped velocity distribution with a large spread in pitch factor is formed as the particles sacrifice axial for rotational momentum. Satellites have observed that the AKR is emitted and extends down to the local electron cyclotron frequency with peaks in frequency at ~300kHz, powers ~10 9 W and with emission efficiency ~1% of the total precipitated electron kinetic energy. Theory has shown this type of distribution to be unstable to cyclotron emissions in the X-mode [1].
AbstractList The auroral density cavity (a region of partial plasma depletion situated at an altitude of around 3200km at the Earth's pole) has been studied to have a background plasma density ~10 6 m -3 , and plasma frequency ~9kHz. Auroral Kilometric Radiation (AKR) is produced when particles descend through this region and are magnetically compressed as they approach the Earth's magnetosphere and through conservation of the magnetic moment, a horseshoe shaped velocity distribution with a large spread in pitch factor is formed as the particles sacrifice axial for rotational momentum. Satellites have observed that the AKR is emitted and extends down to the local electron cyclotron frequency with peaks in frequency at ~300kHz, powers ~10 9 W and with emission efficiency ~1% of the total precipitated electron kinetic energy. Theory has shown this type of distribution to be unstable to cyclotron emissions in the X-mode [1].
Author Cairns, R. A.
Gillespie, K. M.
Whyte, C. G.
Speirs, D. C.
Robertson, C. W.
Phelps, A. D. R.
Ronald, K.
Vorgul, I.
McConville, S. L.
Matheson, K.
King, M.
Kellett, B. J.
Bingham, R.
Koepke, M. E.
Cross, A. W.
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  organization: Dept. of Phys., Univ. of Strathclyde, Glasgow, UK
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  surname: Kellett
  fullname: Kellett, B. J.
  organization: Space Phys. Div., Rutherford Appleton Lab., Didcot, UK
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Snippet The auroral density cavity (a region of partial plasma depletion situated at an altitude of around 3200km at the Earth's pole) has been studied to have a...
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StartPage 2P-71
SubjectTerms Cyclotrons
Earth
Educational institutions
Laboratories
Magnetosphere
Physics
Plasmas
Title Laboratory experiment to investigate the impact of background plasma on cyclotron emission
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