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  • We investigate intense whistler-mode chorus emissions which occurred during the geomagnetic storm on 31 March 2001. We use multipoint measurements obtained by the Cluster spacecraft in the premidnight equatorial region outside the plasmasphere at a radial distance of 4 Earth radii (L = 4.0 - 4.2). Observed spatio-temporal variations of the direction of the Poynting flux manifest a consistent pattern: the central position of the chorus source fluctuates at time scales of minutes within 1000-2000 km of the geomagnetic equator. We demonstrate that estimates of the electromagnetic planarity can be used to characterize the extent of the source, obtaining a range of 3000-5000 km. Discrete wave packets of chorus are observed to rise in frequency between 0.13 and 0.5 of the local electron cyclotron frequency, at a rate up to 20 kHz/s, having the maximum peak amplitudes of 20 mV/m.We observe a fine structure of subpackets with large amplitudes embedded in the interior of the wave packets. This fine structure
  • We investigate intense whistler-mode chorus emissions which occurred during the geomagnetic storm on 31 March 2001. We use multipoint measurements obtained by the Cluster spacecraft in the premidnight equatorial region outside the plasmasphere at a radial distance of 4 Earth radii (L = 4.0 - 4.2). Observed spatio-temporal variations of the direction of the Poynting flux manifest a consistent pattern: the central position of the chorus source fluctuates at time scales of minutes within 1000-2000 km of the geomagnetic equator. We demonstrate that estimates of the electromagnetic planarity can be used to characterize the extent of the source, obtaining a range of 3000-5000 km. Discrete wave packets of chorus are observed to rise in frequency between 0.13 and 0.5 of the local electron cyclotron frequency, at a rate up to 20 kHz/s, having the maximum peak amplitudes of 20 mV/m.We observe a fine structure of subpackets with large amplitudes embedded in the interior of the wave packets. This fine structure (en)
Title
  • A microscopic and nanoscopic view of storm-time chorus.
  • A microscopic and nanoscopic view of storm-time chorus. (en)
skos:prefLabel
  • A microscopic and nanoscopic view of storm-time chorus.
  • A microscopic and nanoscopic view of storm-time chorus. (en)
skos:notation
  • RIV/68378289:_____/04:04030024!RIV/2004/AV0/A04004/N
http://linked.open.../vavai/riv/strany
  • 1;5, doi: 10.1029/20
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA202/03/0832), P(ME 650), Z(AV0Z3042911)
http://linked.open...iv/cisloPeriodika
  • L02801
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 552967
http://linked.open...ai/riv/idVysledku
  • RIV/68378289:_____/04:04030024
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • magnetospheric physics; plasma waves and instabilities; ring current (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • US - Spojené státy americké
http://linked.open...ontrolniKodProRIV
  • [F17506C68194]
http://linked.open...i/riv/nazevZdroje
  • Geophysical Research Letters
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...ocetUcastnikuAkce
http://linked.open...nichUcastnikuAkce
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 31
http://linked.open...iv/tvurceVysledku
  • Parrot, M.
  • Santolík, Ondřej
  • Gurnett, D. A.
  • Pickett, J. S.
  • Cornilleau-Wehrlin, N.
http://linked.open...n/vavai/riv/zamer
issn
  • 0094-8276
number of pages
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