Planetary wave signatures in the equatorial atmosphere–ionosphere system, and mesosphere- E- and F-region coupling
Upward transport of wave energy and momentum due to gravity, tidal and planetary waves from below and extra-tropics controls the phenomenology of the equatorial atmosphere–ionosphere system. An important aspect of this phenomenology is the development of small- and large-scale structures including t...
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Veröffentlicht in: | Journal of atmospheric and solar-terrestrial physics 2006-02, Vol.68 (3), p.509-522 |
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Format: | Artikel |
Sprache: | eng |
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