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  • Long-term trends in the ionospheric D and E regions have been derived from different ground-based radio propagation experiments. The reflection height observations show decreasing trends resulting in a shrinking of the lower ionosphere and atmosphere during the last decades. The trends of the absorption data., however, are more complex. For a very long LF path with a reflection height below 80 km a positive trend was observed. For LF absorption measurements with reflection heights between about 80 - 90 km negative trends were derived whereas for reflection heights above about 90 km (mainly absorption in the MF and HF ranges) again positive absorption trends were estimated. From ionosonde observations it can be shown that the maximum electron density of the E layer has been increased during the last decades. All these features can qualitatively be explained by an increasing atmospheric greenhouse effect with a strato- and mesospheric cooling as well as a decreasing density of nitric oxide and an increa
  • Long-term trends in the ionospheric D and E regions have been derived from different ground-based radio propagation experiments. The reflection height observations show decreasing trends resulting in a shrinking of the lower ionosphere and atmosphere during the last decades. The trends of the absorption data., however, are more complex. For a very long LF path with a reflection height below 80 km a positive trend was observed. For LF absorption measurements with reflection heights between about 80 - 90 km negative trends were derived whereas for reflection heights above about 90 km (mainly absorption in the MF and HF ranges) again positive absorption trends were estimated. From ionosonde observations it can be shown that the maximum electron density of the E layer has been increased during the last decades. All these features can qualitatively be explained by an increasing atmospheric greenhouse effect with a strato- and mesospheric cooling as well as a decreasing density of nitric oxide and an increa (en)
Title
  • Trends in the ionospheric D and E regions using results of different radio propagation experiments.
  • Trends in the ionospheric D and E regions using results of different radio propagation experiments. (en)
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  • Trends in the ionospheric D and E regions using results of different radio propagation experiments.
  • Trends in the ionospheric D and E regions using results of different radio propagation experiments. (en)
skos:notation
  • RIV/68378289:_____/03:04033523!RIV/2004/AV0/A04004/N
http://linked.open.../vavai/riv/strany
  • X1-X5
http://linked.open...avai/riv/aktivita
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  • P(OC 271.10), Z(AV0Z3042911)
http://linked.open...vai/riv/dodaniDat
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http://linked.open...iv/duvernostUdaju
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  • 631475
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  • RIV/68378289:_____/03:04033523
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  • trends; ionosphere (en)
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http://linked.open...ontrolniKodProRIV
  • [CD30D4900D19]
http://linked.open...v/mistoKonaniAkce
  • Faro [PT]
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  • Oxford
http://linked.open...i/riv/nazevZdroje
  • Communications COST 271: Effects of the upper atmosphere on terrestrial and Earth-space.
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
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http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Laštovička, Jan
  • Bremer, J.
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • Appleton-Rutherford Laboratory
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