Self-organization and nonlocal nature of geophysical turbulence and planetary boundary layers
The classical paradigm of the theory of turbulence states that any turbulent flow can be considered as a superposition of the fully organized mean motion and the fully chaotic turbulence is characterized by the direct energy cascade (from larger to smaller eddies). Accordingly, the key tools for mod...
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| Autor principal: | |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2010-12-01
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| coleção: | Геофизический журнал |
| Acesso em linha: | https://journals.uran.ua/geofizicheskiy/article/view/117456 |
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