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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...
Wedi'i Gadw mewn:
| Cyhoeddwyd yn: | J Geophys Res Atmos |
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| Prif Awduron: | , , , , |
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
John Wiley and Sons Inc.
2018
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| Pynciau: | |
| Mynediad Ar-lein: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5856071/ https://ncbi.nlm.nih.gov/pubmed/29576994 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2017JD027440 |
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