Small-scale structures in common-volume meteor wind measurements

Observational differences occur when different techniques are used for measuring mesospheric winds because the different instruments observe different physical quantities to infer the wind velocity, and have differing time and space resolution. The AMOR meteor wind radar near Christchurch, New Zeala...

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Veröffentlicht in:	Journal of atmospheric and solar-terrestrial physics 2006-01, Vol.68 (3), p.317-322
Hauptverfasser:	Fraser, G.J., Marsh, S.H., Baggaley, W.J., Bennett, R.G.T., Lawrence, B.N., McDonald, A.J., Plank, G.E.
Format:	Artikel
Sprache:	eng
Schlagworte:	Common-volume Earth, ocean, space Exact sciences and technology External geophysics Meteor Physics of the high neutral atmosphere Physics of the ionosphere Physics of the magnetosphere Radar Wind
Online-Zugang:	Volltext
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