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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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Bibliographic Details
Date:2010
Main Author: Zilitinkevich, S. S.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2010
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/117456
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal

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