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  • Various external factors of solar origin like solar activity (solar cycle, 27-day variation etc.), geomagnetic storms and other solar wind-related phenomena, and changes of fluxes of high-energy particles can potentially affect the ozone layer. Here we examine the effects of Forbush decreases and other decreases of the galactic cosmic ray (GCR) flux on the columnar ozone content (= total ozone) at higher middle latitudes near 50 N. The Forbush decreases usually occur together with geomagnetic storms and relatively often together wiyh solar proton events (SPEs). Then it is difficult, if not impossible, to distinguish between the effects of geomagnetic storms, SPEs and Forbush decreases and other decreases of GCR flux. Therefore we present here the result of investigations of the effects Forbush decreases and other substantial decreases of the GCR flux on the total ozone for events when there was no geomagnetic storm. Due to dominance of summertime events in the selected data set, very weak if any effec
  • Various external factors of solar origin like solar activity (solar cycle, 27-day variation etc.), geomagnetic storms and other solar wind-related phenomena, and changes of fluxes of high-energy particles can potentially affect the ozone layer. Here we examine the effects of Forbush decreases and other decreases of the galactic cosmic ray (GCR) flux on the columnar ozone content (= total ozone) at higher middle latitudes near 50 N. The Forbush decreases usually occur together with geomagnetic storms and relatively often together wiyh solar proton events (SPEs). Then it is difficult, if not impossible, to distinguish between the effects of geomagnetic storms, SPEs and Forbush decreases and other decreases of GCR flux. Therefore we present here the result of investigations of the effects Forbush decreases and other substantial decreases of the GCR flux on the total ozone for events when there was no geomagnetic storm. Due to dominance of summertime events in the selected data set, very weak if any effec (en)
Title
  • Cosmic rays and total ozone at higher middle latitudes.
  • Cosmic rays and total ozone at higher middle latitudes. (en)
skos:prefLabel
  • Cosmic rays and total ozone at higher middle latitudes.
  • Cosmic rays and total ozone at higher middle latitudes. (en)
skos:notation
  • RIV/68378289:_____/03:04033543!RIV/2004/AV0/A04004/N
http://linked.open.../vavai/riv/strany
  • 2139;2144
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(KSK3012103)
http://linked.open...iv/cisloPeriodika
  • 9
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
  • 602321
http://linked.open...ai/riv/idVysledku
  • RIV/68378289:_____/03:04033543
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • cosmic rays; ozone (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • GB - Spojené království Velké Británie a Severního Irska
http://linked.open...ontrolniKodProRIV
  • [A63664FD4B85]
http://linked.open...i/riv/nazevZdroje
  • Advances in space research
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
  • Križan, Peter
  • Laštovička, Jan
  • Kudela, K.
issn
  • 0273-1177
number of pages
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