Laboratory and theoretical modeling of air-sea momentum transfer under severe wind conditions

被引：63

作者：

Troitskaya, Y. I. ^{[1
,2
]}

Sergeev, D. A. ^{[1
,2
]}

Kandaurov, A. A. ^{[1
,2
]}

Baidakov, G. A. ^{[1
,2
]}

Vdovin, M. A. ^{[1
,2
]}

Kazakov, V. I. ^{[1
,2
]}

机构：

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

[2] Lobachevsky State Univ Nizhni Novgorod, Radiophys Dept, Nizhnii Novgorod, Russia

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS | 2012年 / 117卷

关键词：

ATMOSPHERIC BOUNDARY-LAYER; FLOW SEPARATION; TROPICAL CYCLONES; DRAG COEFFICIENT; WAVE GENERATION; HURRICANE WINDS; SURFACE-WAVES; DYNAMICS; STRESS; SPRAY;

D O I：

10.1029/2011JC007778

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

The laboratory experiments on investigation of aerodynamic resistance of the waved water surface under severe wind conditions (up to U-10 approximate to 40 m s(-1)) were carried out, complemented by measurements of the wind-wave spectra. The tendency to saturation of the surface drag was observed for wind speeds exceeding 25 m s(-1), accompanied by the saturation of wind-wave slopes. The effect of surface drag saturation can be explained quantitatively within the quasi-linear model of the air boundary layer above the waved water surface, when the contribution of the short-wave part of the wind-wave spectrum to aerodynamic resistance of the water surface is taken into account.

引用

页数：13

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