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  • The projection of the plasmapause magnetic-field lines to low altitudes, where the light-ion chemistry is dominated by O+, tends to occur near the minimum electron density in the main (midlatitude) electron density trough at night. With increasing altitude in the trough, where H+ emerges as the dominant ion on the low-latitude boundary, we have found cases where the plasmapause fieldlines are located on the sharp low-latitude side of the trough as expected if this topside ionosphere H+ distribution varies in step with the plasmapause gradient in the distant plasmasphere. These conclusions are based on near-equatorial crossings of the plasmapause (corresponding to the steep gradient in the dominant species H+) by the Explorer-45 satellite as determined from electric-field measurements by Maynard and Cauffman in the early 1970s and ISIS-2 ionospheric topside-sounder measurements. The former data have now been converted to digital form and made available at http://nssdcftp.gsfc.nasa.gov.
  • The projection of the plasmapause magnetic-field lines to low altitudes, where the light-ion chemistry is dominated by O+, tends to occur near the minimum electron density in the main (midlatitude) electron density trough at night. With increasing altitude in the trough, where H+ emerges as the dominant ion on the low-latitude boundary, we have found cases where the plasmapause fieldlines are located on the sharp low-latitude side of the trough as expected if this topside ionosphere H+ distribution varies in step with the plasmapause gradient in the distant plasmasphere. These conclusions are based on near-equatorial crossings of the plasmapause (corresponding to the steep gradient in the dominant species H+) by the Explorer-45 satellite as determined from electric-field measurements by Maynard and Cauffman in the early 1970s and ISIS-2 ionospheric topside-sounder measurements. The former data have now been converted to digital form and made available at http://nssdcftp.gsfc.nasa.gov. (en)
Title
  • Altitude variation of the plasmapause signature in the main ionospheric trough
  • Altitude variation of the plasmapause signature in the main ionospheric trough (en)
skos:prefLabel
  • Altitude variation of the plasmapause signature in the main ionospheric trough
  • Altitude variation of the plasmapause signature in the main ionospheric trough (en)
skos:notation
  • RIV/68378289:_____/09:00338200!RIV10-AV0-68378289
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA300420603), Z(AV0Z30420517)
http://linked.open...iv/cisloPeriodika
  • 16
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
  • 302584
http://linked.open...ai/riv/idVysledku
  • RIV/68378289:_____/09:00338200
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Plasmapause; Ionosphere; Midlatitude Trough (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [08B59723E6C6]
http://linked.open...i/riv/nazevZdroje
  • Journal of Atmospheric and Solar-Terrestrial Physics
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 71
http://linked.open...iv/tvurceVysledku
  • Truhlík, Vladimír
  • Benson, R. F.
  • Bilitza, D.
  • Grebowsky, J. M.
  • Webb, P. A.
http://linked.open...ain/vavai/riv/wos
  • 000271249000009
http://linked.open...n/vavai/riv/zamer
issn
  • 1364-6826
number of pages
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