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Transition from geostrophic turbulence to inertia–gravity waves in the atmospheric energy spectrum

Midlatitude fluctuations of the atmospheric winds on scales of thousands of kilometers, the most energetic of such fluctuations, are strongly constrained by the Earth’s rotation and the atmosphere’s stratification. As a result of these constraints, the flow is quasi-2D and energy is trapped at large...

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Publicat a:Proc Natl Acad Sci U S A
Autors principals: Callies, Jörn, Ferrari, Raffaele, Bühler, Oliver
Format: Artigo
Idioma:Inglês
Publicat: National Academy of Sciences 2014
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Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC4260586/
https://ncbi.nlm.nih.gov/pubmed/25404349
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1410772111
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