Gravity Wave Dynamics in a Mesospheric Inversion Layer: 1. Reflection, Trapping, and Instability Dynamics

An anelastic numerical model is employed to explore the dynamics of gravity waves (GWs) encountering a mesosphere inversion layer (MIL) having a moderate static stability enhancement and a layer of weaker static stability above. Instabilities occur within the MIL when the GW amplitude approaches tha...

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Detalles Bibliográficos
Autores principales: Fritts, David C., Laughman, Brian, Wang, Ling, Lund, Thomas S., Collins, Richard L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2018
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5856071/
https://www.ncbi.nlm.nih.gov/pubmed/29576994
http://dx.doi.org/10.1002/2017JD027440

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5856071/
https://www.ncbi.nlm.nih.gov/pubmed/29576994
http://dx.doi.org/10.1002/2017JD027440

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