Statistical properties of the atmospheric turbulent boundary layer over steep surface waves

A new method of digital optical anemometry (Particle Image Velocimetry, PIV) of turbulent flows is suggested and implemented in the laboratory; it is based on the use of continuous laser radiation and high-speed video photography, providing continuous statistical ensembles of flow velocity fields. A...

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Veröffentlicht in:Doklady earth sciences 2010-07, Vol.433 (1), p.922-926
Hauptverfasser: Troitskaya, Yu. I., Sergeev, D. A., Ermakova, O. S., Balandina, G. N.
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container_issue 1
container_start_page 922
container_title Doklady earth sciences
container_volume 433
creator Troitskaya, Yu. I.
Sergeev, D. A.
Ermakova, O. S.
Balandina, G. N.
description A new method of digital optical anemometry (Particle Image Velocimetry, PIV) of turbulent flows is suggested and implemented in the laboratory; it is based on the use of continuous laser radiation and high-speed video photography, providing continuous statistical ensembles of flow velocity fields. Application of the method to the study of wind field over waves has allowed us to perform, for the first time, direct measurements of velocity fields, averaged over turbulent pulsations induced by waves in the air flow. The experiments demonstrated that the velocity fields, averaged over the turbulent pulsations, are nonseparated even in the case of steep and breaking waves, when separation of the flow from the wave crests in the instantaneous fields is observed. Based on comparison with the experimental data, it is shown that the average wind fields over waves are described well quantitatively in the framework of semiempirical closure models of turbulence.
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subjects Air flow
Analysis
Atmospheric boundary layer
Boundary layers
Earth and Environmental Science
Earth Sciences
Flow velocity
Lasers
Nuclear radiation
Oceanology
Optics
Scientific apparatus & instruments
Turbulence
Wave crest
Wind
title Statistical properties of the atmospheric turbulent boundary layer over steep surface waves
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