Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers

The processes of momentum and heat transfer between ocean and atmosphere in the boundary layer were investigated within laboratory modeling for a wide range of wind speed and surface wave including hurricane conditions. Experiments were carried out on the Wind-Wave Flume of the Large Thermostratifie...

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Main Authors: Sergeev Daniil, Kandaurov Alexander, Troitskaya Yuliya, Vdovin Maxim
Format: Article
Language:English
Published: EDP Sciences 2017-01-01
Series:EPJ Web of Conferences
Online Access:https://doi.org/10.1051/epjconf/201714302100
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spelling doaj-384b996b5dee4d0aacb5a268c1013cc12021-08-02T01:13:26ZengEDP SciencesEPJ Web of Conferences2100-014X2017-01-011430210010.1051/epjconf/201714302100epjconf_efm2017_02100Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layersSergeev DaniilKandaurov AlexanderTroitskaya YuliyaVdovin MaximThe processes of momentum and heat transfer between ocean and atmosphere in the boundary layer were investigated within laboratory modeling for a wide range of wind speed and surface wave including hurricane conditions. Experiments were carried out on the Wind-Wave Flume of the Large Thermostratified Tank of IAP RAS. A special net located under the surface at different depths allows to vary parameters of surface waves independently on wind parameters. Theory of self-similarity of air flow parameters in the flume was used to calculate values aerodynamic and heat transfer coefficients from the measured velocity and temperature profiles by Pito and hotfilm gauges respectively. Simultaneous measurements of surface elevation with system wire allow to obtain spectra and integral parameters of waves. It was demonstrated that in contrast to the drag coefficient, heat transfer coefficient is virtually independent of wind speed and wave parameters to the moment of the beginning of spray generation and then increases rapidly.https://doi.org/10.1051/epjconf/201714302100
collection DOAJ
language English
format Article
sources DOAJ
author Sergeev Daniil
Kandaurov Alexander
Troitskaya Yuliya
Vdovin Maxim
spellingShingle Sergeev Daniil
Kandaurov Alexander
Troitskaya Yuliya
Vdovin Maxim
Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
EPJ Web of Conferences
author_facet Sergeev Daniil
Kandaurov Alexander
Troitskaya Yuliya
Vdovin Maxim
author_sort Sergeev Daniil
title Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
title_short Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
title_full Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
title_fullStr Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
title_full_unstemmed Laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
title_sort laboratory modelling of the transfer processes between the ocean and atmosphere in the boundary layers
publisher EDP Sciences
series EPJ Web of Conferences
issn 2100-014X
publishDate 2017-01-01
description The processes of momentum and heat transfer between ocean and atmosphere in the boundary layer were investigated within laboratory modeling for a wide range of wind speed and surface wave including hurricane conditions. Experiments were carried out on the Wind-Wave Flume of the Large Thermostratified Tank of IAP RAS. A special net located under the surface at different depths allows to vary parameters of surface waves independently on wind parameters. Theory of self-similarity of air flow parameters in the flume was used to calculate values aerodynamic and heat transfer coefficients from the measured velocity and temperature profiles by Pito and hotfilm gauges respectively. Simultaneous measurements of surface elevation with system wire allow to obtain spectra and integral parameters of waves. It was demonstrated that in contrast to the drag coefficient, heat transfer coefficient is virtually independent of wind speed and wave parameters to the moment of the beginning of spray generation and then increases rapidly.
url https://doi.org/10.1051/epjconf/201714302100
work_keys_str_mv AT sergeevdaniil laboratorymodellingofthetransferprocessesbetweentheoceanandatmosphereintheboundarylayers
AT kandaurovalexander laboratorymodellingofthetransferprocessesbetweentheoceanandatmosphereintheboundarylayers
AT troitskayayuliya laboratorymodellingofthetransferprocessesbetweentheoceanandatmosphereintheboundarylayers
AT vdovinmaxim laboratorymodellingofthetransferprocessesbetweentheoceanandatmosphereintheboundarylayers
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