Fine structure of the turbulent atmospheric boundary layer over the water surface

被引：4

作者：

Troitskaya, Yu. I. ^{[1
]}

Sergeev, D. A. ^{[1
]}

Ermakova, O. S. ^{[1
]}

Balandina, G. N. ^{[1
]}

机构：

[1] Russian Acad Sci, Inst Appl Phys, Nizhnii Novgorod 603950, Russia

来源：

IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS | 2010年 / 46卷 / 01期

基金：

俄罗斯基础研究基金会;

关键词：

FOLLOWER FIELD-MEASUREMENTS; INPUT SPECTRAL-FUNCTION; AIR-FLOW; COORDINATE SYSTEM; NUMERICAL-MODEL; SHEAR FLOWS; WIND-INPUT; WAVES; GENERATION; PARAMETERIZATION;

D O I：

10.1134/S0001433810010147

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

In this paper, the results of a laboratory experiment on investigating the wind-velocity field over a water surface using the PIV method are described. The use of a rapid CCD-camera made it possible to perform a detailed study of the eddy structure of airflow. We have measured the velocity fields over a flat plate by wind waves and waves induced by a wave generator. The model of a turbulent boundary layer over a rough surface was directly verified. It has been shown that the wind-velocity profiles over waves obtained by averaging the instantaneous fields over the ensemble of samples and horizontal coordinate are satisfactorily consistent with the profiles calculated within the frameworks of the model of wind flow over rough water surface.

引用

页码：109 / 120

页数：12

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