Absorption of waves by large-scale winds in stratified turbulence

The atmosphere is a nonlinear stratified fluid in which internal gravity waves are present. These waves interact with the flow, resulting in wave turbulence that displays important differences with the turbulence observed in isotropic and homogeneous flows. We study numerically the role of these wav...

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Detalles Bibliográficos
Autores principales: Clark Di Leoni, P., Mininni, P.D.
Formato: JOUR
Materias:
Dispersions
Turbulence
Current theories
Dispersion relations
Homogeneous flow
Horizontal layers
Internal gravity waves
Large-scale flows
Stratified fluid
Stratified turbulence
Wind
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_15393755_v91_n3_p_ClarkDiLeoni
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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