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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2017-01-01
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Series: | EPJ Web of Conferences |
Online Access: | https://doi.org/10.1051/epjconf/201714302100 |
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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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1721245024653410304 |