Atmospheric Tidal Oscillations: An Analysis of the Mechanics

An approximate formula for the equivalent depth of a compressible atmosphere is developed and shows that Coriolis forces dominate the diurnal tide causing it to have a small scale depth. It follows that either the diurnal motion field is confined to the vicinity of the heating and is rather feeble,...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Proceedings of the Royal Society of London. Series A, Mathematical and physical sciences Mathematical and physical sciences, 1965-11, Vol.288 (1415), p.564-574
1. Verfasser:	Green, J. S. A.
Format:	Artikel
Sprache:	eng
Schlagworte:	A Discussion on Some Aspects of the Stratosphere, Mesosphere and Lower Thermosphere Amplitude Atmospherics Boundary conditions Density Fracture mechanics Kinetics Oxygen Ozone Tidal interaction Wavelengths
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!