On the role of the stratosphere in the process of overflow of mesoscale mountains
A 2-D, two- and three-layer stratified airflow over a mountain of arbitrary shape is considered on the assumptions that upstream wind velocity and static stability within each layer are constant (Long's model). The stratosphere is simulated by an infinitely deep upper layer with enhanced st...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2005-12-01
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| Series: | Annales Geophysicae |
| Online Access: | https://www.ann-geophys.net/23/3407/2005/angeo-23-3407-2005.pdf |