Small-scale gravity waves in the upper mesosphere and lower thermosphere generated by deep tropical convection

A time-dependent, nonlinear, fully compressible, axisymmetric, f-plane, numerical model is used to simulate the generation of small-scale gravity waves in the upper mesosphere and lower thermosphere by intense deep convection in the troposphere. The simulations show that major convective storms in t...

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Veröffentlicht in:	Journal of Geophysical Research. D. Atmospheres 2001-12, Vol.106 (D23), p.31
Hauptverfasser:	Walterscheid, R L, Schubert, G, Brinkman, D G
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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