Different regimes for water wave turbulence

We present an experimental study on gravity capillary wave turbulence in water. By using space-time resolved Fourier transform profilometry, the behavior of the wave energy density |ηk,ω|2 in the 3D (k,ω) space is inspected for various forcing frequency bandwidths and forcing amplitudes. Depending o...

Descripción completa

Detalles Bibliográficos
Publicado: 2011
Materias:
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00319007_v107_n21_p_Cobelli
http://hdl.handle.net/20.500.12110/paper_00319007_v107_n21_p_Cobelli
Aporte de:
id paper:paper_00319007_v107_n21_p_Cobelli
record_format dspace
spelling paper:paper_00319007_v107_n21_p_Cobelli2023-06-08T14:57:56Z Different regimes for water wave turbulence Bandwidth Profilometry Water waves Wave energy conversion Forcing amplitudes Forcing frequencies Fourier transform profilometry Gravity capillary waves In-laboratory experiments Spectral slopes Wave energy density Wave turbulence Turbulence We present an experimental study on gravity capillary wave turbulence in water. By using space-time resolved Fourier transform profilometry, the behavior of the wave energy density |ηk,ω|2 in the 3D (k,ω) space is inspected for various forcing frequency bandwidths and forcing amplitudes. Depending on the bandwidth, the gravity spectral slope is found to be either forcing dependent, as classically observed in laboratory experiments, or forcing independent. In the latter case, the wave spectrum is consistent with the Zakharov-Filonenko cascade predicted within wave turbulence theory. © 2011 American Physical Society. 2011 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00319007_v107_n21_p_Cobelli http://hdl.handle.net/20.500.12110/paper_00319007_v107_n21_p_Cobelli
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Bandwidth
Profilometry
Water waves
Wave energy conversion
Forcing amplitudes
Forcing frequencies
Fourier transform profilometry
Gravity capillary waves
In-laboratory experiments
Spectral slopes
Wave energy density
Wave turbulence
Turbulence
spellingShingle Bandwidth
Profilometry
Water waves
Wave energy conversion
Forcing amplitudes
Forcing frequencies
Fourier transform profilometry
Gravity capillary waves
In-laboratory experiments
Spectral slopes
Wave energy density
Wave turbulence
Turbulence
Different regimes for water wave turbulence
topic_facet Bandwidth
Profilometry
Water waves
Wave energy conversion
Forcing amplitudes
Forcing frequencies
Fourier transform profilometry
Gravity capillary waves
In-laboratory experiments
Spectral slopes
Wave energy density
Wave turbulence
Turbulence
description We present an experimental study on gravity capillary wave turbulence in water. By using space-time resolved Fourier transform profilometry, the behavior of the wave energy density |ηk,ω|2 in the 3D (k,ω) space is inspected for various forcing frequency bandwidths and forcing amplitudes. Depending on the bandwidth, the gravity spectral slope is found to be either forcing dependent, as classically observed in laboratory experiments, or forcing independent. In the latter case, the wave spectrum is consistent with the Zakharov-Filonenko cascade predicted within wave turbulence theory. © 2011 American Physical Society.
title Different regimes for water wave turbulence
title_short Different regimes for water wave turbulence
title_full Different regimes for water wave turbulence
title_fullStr Different regimes for water wave turbulence
title_full_unstemmed Different regimes for water wave turbulence
title_sort different regimes for water wave turbulence
publishDate 2011
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00319007_v107_n21_p_Cobelli
http://hdl.handle.net/20.500.12110/paper_00319007_v107_n21_p_Cobelli
_version_ 1768542209812987904