A tidal theory of the ionospheric intermediate layer

書誌事項

公開日
1973-03
権利情報
  • https://www.elsevier.com/tdm/userlicense/1.0/
  • https://www.elsevier.com/legal/tdmrep-license
DOI
  • 10.1016/0021-9169(73)90034-2
公開者
Elsevier BV

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説明

Abstract The dynamical perturbations on the ionizations in middle altitudes at night were studied by solving the time-dependent continuity equation involving the charge transport effects. The propagating (2.4) mode of the solar semi-diurnal atmospheric tide is found to be the dominant cause of the intermediate layers at night. The vertical drift of the ionizations by the S q electric field seems to modify also the altitude variation of the intermediate layer during the course of night.

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